Upload
others
View
3
Download
0
Embed Size (px)
Citation preview
THE USE OF GASIFICATION ASH IN CEMENT AND
CONCRETE
HANLI DU PLESSIS
A d isser ta t ion submit ted in par t ia l fu l f i l lment for the degree of
MASTER OF ENGINEERING (STRUCTURAL ENGINEERING)
In the
FACULTY OF ENGINEERING
UNIVERSITY OF PRETORIA
November 2005
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
SUMMARY
THE USE OF GASIFICATION ASH IN CEMENT AND
CONCRETE
H DU PLESSIS
Superv isor : P ro fesso r E .P . Kea rs l ey
Depar tm ent : C i v i l Eng inee r i ng
Univers i ty : Un i ve r s i t y o f P re t o r i a
Degree : Mas te r o f Eng inee r i ng (S t ruc tu ra l Eng inee r i ng )
Cemen t i s an essen t i a l ma te r i a l i n t oday ’ s soc i e t y because , as a ma jo r
cons t i t uen t o f conc re te , i t f o rms a f u ndamen ta l e l emen t o f any h ous ing
o r i n f r as t ruc tu re deve lopme n t . The chem ica l p rocess o f mak ing cemen t
c l i n ke r p roduces CO 2 , a ma jo r g reenhouse gas con t r i bu t i ng t o c l ima te
change . Th i s makes i t impe ra t i ve f o r us t o f i nd ways o f us i ng t h i s
r esou rce more e f f i c i en t l y .
Us ing was te f r om o the r i ndus t r i es , as a r aw ma te r i a l i s a huge
oppo r tun i t y f o r t he cemen t i ndus t r y t o r educe i t s env i r onmen ta l impac t .
Cemen t ex tende rs a re used as a subs t i t u te f o r some o f t he Po r t l and
cemen t i n conc re te . The re asons f o r t he use o f ex tend e rs , i s a g row ing
awa reness o f t he eng inee r i ng , econom ica l and eco log i ca l bene f i t s and
t he va r i e t y o f use fu l enhancemen ts , wh i ch t hey g i ve t o t he conc re te
p rope r t i es .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
The a im o f t he r e sea rch i s t o de te rm ine whe the r a ga s i f i ca t i on ash can
be used as a cemen t ex tende r i n conc re te . I n t h i s s tudy de ta i l o f t he
manu fac tu r i ng o f Po r t l and cemen t (PC) , cemen t c l asses and t he
hyd ra t i on o f cemen t w i l l be d i scussed . Cons ide ra t i on w i l l be g i ven t o
p rope r t i es l i ke t he op t im i sa t i on o f su l pha te and f i neness o f cemen t .
The pa r t i c l e s i ze d i s t r i bu t i on i s d i s cussed w i t h spec i f i c r e f e rence t o t he
Ros in -Rammle r d i s t r i bu t i on f unc t i on . The use o f coa l combus t i on by -
p roduc t s , spec i f i ca l l y f l y ash , i n conc re te w i l l be d i scussed .
Cons ide ra t i on w i l l be g i ven t o p rope r t i es l i ke shape , pa r t i c l e s i ze ,
m ine ra l og i ca l and chem ica l compos i t i on , du rab i l i t y and t he chem ica l
r equ i r emen ts f o r us i ng f l y as h as a cemen t ex tende r .
The phys i ca l p rope r t i es o f gas i f i ca t i on ash i nd i ca ted t ha t t he
gas i f i ca t i on ash , g r i nded sepa ra te and i n t e rg round had s im i l a r pa r t i c l e
s i ze d i s t r i bu t i ons . The chem ica l and m ine ra l og i ca l compos i t i on o f a
gas i f i ca t i on ash samp le was i nves t i ga ted , and i t was f ound t ha t
gas i f i ca t i on ash has an angu la r shape and a s im i l a r chem ica l
compos i t i on as f l y ash .
The chem ica l r equ i r emen ts o f t he gas i f i ca t i on ash mee t t he ma jo r i t y o f
t he r equ i r emen ts spec i f i ed f o r cemen t ex tende rs . Whe re l im i t s a re
exceeded i t i s by a ve r y na r row marg in .
The e f f ec t o f a gas i f i ca t i on ash on t he sho r t and l ong t e rm p ro pe r t i es
o f conc re te o f bo th i n t e rb l end ing and i n t e rg r i nd i ng was i nves t i ga ted .
The use o f gas i f i ca t i on as h as cemen t ex tende r does no t have a
nega t i ve impac t on t he s t r eng th deve l opmen t o f conc re te . The re was no
reduc t i on i n t he t ens i l e s t r eng th o f conc re te . Gas i f i ca t i on ash does no t
have a d e t r imen ta l e f f ec t on s t i f f ness o f conc re te , and d i d no t sh r i nk o r
c reep s i gn i f i can t l y mo re t han conc re te con ta i n i ng f l y ash .
The po ros i t y and pe rmeab i l i t y does no t i n c rease when gas i f i ca t i on ash
i s used as a cemen t ex tende r . Gas i f i ca t i on as h shou ld t he re fo re no t
dec rease t he du rab i l i t y o f conc re te .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
SAMEVATTING VAN
DIE BENUTTING VAN GASIFIKASIE-AS IN SEMENT EN
BETON
H DU PLESSIS
Promoto r : P ro fesso r E .P . Kea rs l ey
Depar te ment : S i v i e l e I ngen ieu rswese
Univers i te i t : Un i ve r s i t e i t van P re to r i a
Graad: Mag i s te r van I ngen ieu rwese (S t ruk tuu r
I ngen ieu rswese )
Semen t i s ‘ n be lang r i ke ma te r i aa l i n d i e hedendaagse gemeenskap
wan t as ‘ n hoo f ve r vang ingsma te r i aa l i n be ton , vo rm d i t ‘ n be lang r i ke
e l emen t van e n ige behu i s i ng o f i n f r as t r uk tuu r on tw i kke l i ng . D ie
chem iese p roses t ydens d i e ve r vaa rd i g i ng van semen t s t e l CO 2 , ‘ n gas
wa t l e i t o t k l imaa t sve rande r i ng , v r y . H ie rd i e aspek maak d i t be l ang r i k
v i r ons om man ie re t e k r y om h ie rd i e b ron mee r e f f ek t i e f t e geb ru i k .
Benu t t i ng van a f va l ma te r i a l e van ande r i ndus t r i eë as a r ou ma te r i aa l
i s a g roo t kans v i r d i e s emen t i n dus t r i e om hu l o mgew ing s impak t e
ve rm inde r . Semen t - ve rvang e rs wo rd geb ru i k as ve rva ng ing v i r ‘ n dee l
van d i e Po r t l and Semen t i n be ton . The redes v i r d i e geb ru i k van
ve rvange rs i s ‘ n g roe iende bewusword ing van d i e i ngen ieu rs
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
ekonom iese en eko log iese voo rd ee l asook d i e ve r ske idenhe id
ve rbe te r i ngs wa t hu l l e byd ra t o t d i e e i enskappe van be ton .
D ie doe l van d i e navo rs i ng i s om te bepaa l o f gas i f i kas i e -as geb ru i k
kan wo rd as ‘ n semen t - ve rvange r i n be ton . I n h i e rd i e s t ud ie wo rd
i n l i g t i ng oo r d i e ve r vaa rd i g i ng van Po r t l and semen t , semen t k l asse en
d i e h i d ras i e van semen t besp reek . Kons ide ras i e wo rd gegee aan
e i enskappe soos d i e op t im i se r i ng van su l f aa t en d i e f ynh e id van
semen t . D ie pa r t i ke l g roo t te ve r sp re i d i ng wo rd besp reek me t spes i f i e ke
ve rwys ing na d i e Ros in -Rammle r ve r sp re i d i ng funks ie . D ie geb ru i k van
s teenkoo l as a f va l p roduk te , spes i f i e k V l i egas , i n be ton wo rd besp reek .
Kons ide ras i e wo rd gegee aan e i enskappe soos vo rm , pa r t i ke l g roo t t e ,
m ine ra l og ie en chem iese sames te l l i ng , duu rsaamhe id en d i e chem iese
ve re i s t es v i r d i e geb ru i k van V l i egas as ‘ n semen t - ve r vange r .
D ie f i s i ese e i enskappe va n gas i f i kas i e -as du i daa rop da t ga s i f i kas i e -
as , apa r t gemaa l en saam gemaa l d i ese l f de pa r t i ke l g roo t t e
ve r sp re i d i ngs he t . D ie chemiese en m ine ra l og iese sames te l l i ng van
gas i f i kas i e -as i s onde rsoek en daa r i s gev i nd da t gas i f i kas i e -as ‘ n
hoek ige vo rm en d i ese l f de sames te l l i ng as v l i egas he t .
The chem iese ve re i s t es v i r gas i f i kas i e as vo l doen aan d i e me e rde rhe id
van d i e ve re i s t es gespes i f i see r v i r semen t - ve r vange rs . Waa r d i e
l im ie te oo rsk re i wo rd i s d i t s l egs me t ‘ n k l e i n ma rg in .
D ie e f f ek van gas i f i kas i e as op d i e ko r t en l ang t e rmyn e i enskappe van
be ton v i r be i de saamgemen g en saamgemaa l i s onde rsoek . D ie geb ru i k
van gas i f i kas i e -as as ‘ n semen t - ve r vange r he t geen nega t i ewe impak
op d i e s te r k t e on tw i kke l i ng van be ton n i e . Daa r was geen ve rm inde r i ng
i n d i e t r eks te r k te van d i e be ton n i e . Gas i f i kas i e -as he t n i e ‘ n nade l i ge
e f f ek op d i e s t y f he id van d i e be ton en he t n i e besonde rs mee r gek r imp
o f k ru i p n i e as be ton me t v l i egas n i e .
D ie po ros i t e i t en pe rmeab i l i t e i t he t n i e ve rmee rde r as gas i f i kas i e -as
geb ru i k wo rd as ‘ n semen t - ve r vang e r n i e . Gas i f i kas i e -as sa l daa rvoo r
n i e d i e duu rsaamhe id van be ton ve rm inde r n i e .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
ACKNOWLEDGEMENT
I w i sh t o exp ress my app re c i a t i on t o t he f o l l ow ing o rgan i za t i ons and
pe rsons who mad e t h i s d i sse r t a t i on poss ib l e .
a ) Saso l Techno logy Resea rch and Deve lopmen t f o r t he dona t i on o f
gas i f i ca t i on ash t es ted i n t h i s i nves t i ga t i on .
b ) P ro fesso r E .P Kea rs l ey , my p romo te r f o r he r gu idance and
suppo r t .
c ) The f o l l ow ing pe rsons f o r t he i r ass i s tance du r i ng t he cou rse o f
s t udy :
M r . D . Mos te r t
M r . H . Ma t j i e
M rs . S . Ve r r yn
M rs . J . Ca l l anan
Pe rsonne l o f t he conc re te l abo ra to r y o f t he C i v i l Eng inee r i ng
depa r tmen t o f t he Un i ve rs i t y o f P re t o r i a .
d ) My f a m i l y and f r i ends f o r t he i r encou ragemen t and suppo r t .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
TABLE OF CONTENTS PAGE
1 . INTRODUCTION 1 -1
1 . 1 Backg round 1 -1
1 .2 Ob jec t i ves o f t he s t udy 1 -2
1 .3 Scope o f t he s t udy 1 -2
1 .4 Me thodo logy 1 -4
1 .5 O rgan i sa t i on o f t he r epo r t 1 -4
2. COM PON ENT S AND P ROP ERTI ES OF P ORTLA N D CE MEN T 2 -1
2 .1 I n t r oduc t i on 2 -1
2 .2 Cemen t Manu fac tu re 2 -1
2 .3 Cemen t C lasses 2 -4
2 .4 Hyd ra t i on o f Po r t l and Ceme n t 2 -5
2 . 4 .1 The hyd ra t i on o f C 3 S and C 2 S 2 - 5
2 . 4 .2 Hyd ra t i on o f C 3 A 2 -8
2 . 4 .3 Hyd ra t i on o f C 4 AF 2 -9
2 .5 Hea t o f Hyd ra t i on 2 -9
2 . 5 .1 Op t im i za t i on o f Cemen t Su lpha te 2 -10
2 .6 Spec i f i c Su r f ace A rea 2 -12
2 .7 Pa r t i c l e s i ze d i s t r i bu t i on 2 -12
2 . 7 .1 Ros in -Rammle r d i s t r i bu t i on f unc t i on 2 -13
2 .8 Conc lus i on 2 -15
3 . COMPOSIT ION AND PROPERTIES OF COAL ASH 3 -1
3 .1 In t roduc t i on 3 -1
3 .2 Coa l Ash 3 -2
3 .3 Pozzo lan i c Reac t ion 3 -4
3 .4 F l y Ash 3 -5
3 .4 .1 Phys ica l P roper t i es 3 -6
3 .4 .2 Chemica l Compos i t i on 3 -7
3 .4 .3 M inera log i ca l Compos i t i on 3 -8
3 .4 .4 Chemica l Spec i f i ca t ions 3 -8
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3 .5 I n f l uence o f f l y ash on t he p rope r t i es o f conc re te 3 -9
3 .5 .1 F resh Conc re te 3 -9
3 .5 .1 .1 Wa te r Demand 3 -10
3 .5 .1 .2 Workab i l i t y 3 -11
3 .5 .2 Ha rdened Conc re te 3 -12
3 .5 .2 .1 Compres s i ve S t reng th Deve lopmen t 3 -12
3 .5 .2 .2 F l exu ra l S t r eng th 3 -15
3 .5 .2 .3 Modu lus o f E l as t i c i t y 3 -16
3 .5 .2 .4 D ry i ng Sh r i nkage 3 -17
3 .5 .2 .5 C reep 3 -18
3 .6 Durab i l i t y o f Conc re te 3 -19
3 .6 .1 Poros i t y 3 -19
3 .6 .2 Pe rmeab i l i t y 3 -19
3 .7 Advan tag es o f us i ng F l y ash i n Conc re te 3 -20
3 .8 Conc lus ion 3 -21
4 . E XPERI M ENTAL P ROGRA MME A ND TEST PROCE DURES
FOR C EM ENT 4 -1
4 . 1 I n t r oduc t i on 4 -1
4 .2 P repa ra t i on o f ma te r i a l s 4 -1
4 .3 Phys i ca l and chem ica l p rope r t i es o f gas i f i ca t i on ash 4 -4
4 .3 .1 Pa r t i c l e s i ze d i s t r i bu t i on 4 -4
4 .3 .1 .1 Pa r t i c l e s i ze d i s t r i bu t i on pa rame te r s 4 -4
4 .3 .1 .2 Ros in -Rammle r pa r t i c l e s i ze
d i s t r i bu t i on pa rame te r s 4 -5
4 .3 .1 .3 Pa r t i c l e s i ze d i s t r i bu t i on pa rame te r s 4 -7
4 .3 .2 Spec i f i c su r f ace a rea 4 -8
4 .3 .3 Scann ing e l ec t r on m i c roscopy (SEM) 4 -9
4 .3 .4 X - ra y f l u o rescence spec t roscopy (XRF) 4 -9
4 .3 .5 X - ra y d i f f r ac t i on spec t roscopy (XRD) 4 -10
4 .4 S tanda rd t es t s f o r cemen t i t i ous ma te r i a l s 4 -10
4 .4 .1 Su lphu r t r i o x i de con ten t
(SANS 50 196 -2 :1994 / SABS EN 196 -2 :1994 ) 4 -11
4 .4 .2 Loss on Ign i t i on
(SANS 50 196 -2 :1994 / SABS EN 196 -2 :1994 ) 4 -11
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
4 . 4 .3 F ree wa te r con ten t
(SANS 61 51 :1989 / SABS 11 51 :1989 ) 4 -12
4 .4 .4 Tes t f o r f i neness o f cemen t and Po r t l and cemen t
ex tende rs (SANS 6157 :2002 / SABS 1157 :2002 ) 4 -12
4 . 4 .5 Wa te r r equ i r emen t
(SANS 61 56 :1989 / SABS SM 1156 :1989 ) 4 -12
4 . 4 .6 S t r eng th f ac to r t es t
(SANS 50 196 -1 :1994 / SABS EN 196 -1 :1994 ) 4 -15
4 .4 .7 Soundness
(SANS 50 196 -3 :1994 / SABS EN 196 -3 :1994 ) 4 -17
4 .4 .8 Re la t i ve dens i t y ( LSA Me th od ) 4 -18
4 .5 Fac to r s Inves t i ga ted by Ca s t i ng Mo r ta r P r i sms 4 -18
4 .5 .1 D i f f e ren t G r i nd i ng T imes 4 -18
4 .5 .2 D i f f e ren t Gypsu m Pe rcen tages 4 -19
4 .5 .3 I so the rma l Conduc t i on Ca lo r ime t r y 4 -20
4 .5 .4 D i f f e ren t r ep lacemen ts pe rcen tages o f
Gas i f i ca t i on Ash 4 -20
5 . E XPERI M ENTAL P ROGRA MME A ND TEST PROCE DURES
FOR C ON CRETE 5 -1
5 . 1 I n t r oduc t i on 5 -1
5 .2 M i x des ign f o r conc re te m i xes 5 -1
5 .3 Tes t Conduc ted on F resh Conc re te M i xes 5 -2
5 .3 .1 S l ump Tes t (SANS 586 / SABS SM 8 2 :1994 ) 5 -2
5 .4 S t reng th Tes t 5 -3
5 .4 .1 Compres s i ve S t reng th Tes t
(SANS 58 63 -1 /SABS 863 -1994 ) 5 -3
5 .4 .2 Sp l i t t i ng Cy l i nde r Tes t f o r Tens i l e S t reng th
(SANS 62 5 :1994 /SABS SM 1253 :1994 ) 5 -4
5 .5 De fo rma t i on and Vo lume Ch ange o f Conc re te 5 -4
5 .5 .1 E -Va lue Tes t 5 -4
5 .5 .2 Sh r i nkage and C reep Tes t (ASTM C 512 -02 ) 5 -6
5 .6 Du rab i l i t y 5 -8
5 .6 .1 Po ros i t y Tes t 5 -8
5 .6 .2 Oxygen Pe rmeab i l i t y Tes t 5 -9
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6 . TEST RESULTS AND D ISCUSSION ON CEMENT TESTS 6 -1
6 . 1 I n t r oduc t i on 6 -1
6 .2 Phys i ca l P rope r t i es 6 -1
6 .2 .1 Pa r t i c l e S i ze D i s t r i bu t i on Tes t 6 -1
6 .2 .2 Shape o f Pa r t i c l es 6 -10
6 .3 Chem ica l P rope r t i es 6 -12
6 .3 .1 XRF 6 -12
6 .3 .2 XRD 6 -14
6 .3 .3 S tanda rd Tes t s f o r Cemen t i t i ous Ma te r i a l s 6 -15
6 .4 E f f ec t o f G r i nd i ng t ime on t he P rope r t i es o f I n t e rb l ended
Gas i f i ca t i on Ash and Ceme n t 6 -16
6 .4 .1 Mo r ta r P r i sm Compress i ve S t reng th 6 -16
6 .4 .2 Mo r ta r P r i sms F lexu ra l S t r eng th 6 -17
6 .4 .3 Pa r t i c l e S i ze D i s t r i bu t i on 6 -19
6 .5 E f f ec t o f G r i nd i ng t ime on t he P rope r t i es o f I n t e rg round
Gas i f i ca t i on Ash and Ceme n t 6 -22
6 .5 .1 Mo r ta r P r i sm Compress i ve S t reng th 6 -22
6 .5 .2 Mo r ta r P r i sm F lexu ra l S t r eng th 6 -23
6 .5 .3 Pa r t i c l e S i ze D i s t r i bu t i on 6 -24
6 .6 E f f ec t o f Gypsu m Con ten t on t he P rope r t i es o f I n t e rg round
Gas i f i ca t i on Ash and Ceme n t 6 -27
6 .6 .1 Mo r ta r P r i sm Compress i ve S t reng th 6 -27
6 .6 .2 Mo r ta r P r i sm F lexu ra l S t r eng th 6 -28
6 .6 .3 Hea t o f Hyd ra t i on 6 -29
6 .7 E f f ec t o f Rep lacemen t Leve l s on t he P rope r t i es o f
I n t e rg round Gas i f i ca t i on Ash and Cemen t 6 -32
6 .7 .1 Mo r ta r P r i sm Compress i ve S t reng th 6 -32
6 .7 .2 Mo r ta r P r i sm F lexu ra l S t r eng th 6 -34
6 .7 .3 Pa r t i c l e S i ze D i s t r i bu t i on 6 -35
6 .8 Compar i son be tween Manu fac tu red and Commerc i a l Cemen t 6 -38
6 .8 .1 Mo r ta r P r i sm Compress i ve S t reng th 6 -38
6 .8 .2 F l exu ra l Mo r ta r P r i sm S t reng ths 6 -39
6 .8 .3 Hea t o f Hyd ra t i on 6 -41
6 .9 Conc lus i on 6 -41
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
7 . TEST RESULTS AND D ISCUSSION ON CONCRETE T ESTS 7 -1
7 . 1 I n t r oduc t i on 7 -1
7 .2 Tes t s Conduc ted on F resh Conc re te 7 -1
7 .2 .1 S l ump Tes t 7 -1
7 .3 S t reng th Tes t s 7 -2
7 .3 .1 Conc re te Cube Co mpress ion Tes t Resu l t s 7 -2
7 .3 .2 Tens i l e S t reng th Resu l t s 7 -3
7 .4 De fo rma t i on and Vo lume Ch ange o f Conc re te 7 -4
7 .4 .1 E - va lue t es t r esu l t s 7 -4
7 .4 .2 Sh r i nkage and C reep Tes t 7 -6
7 .5 Du rab i l i t y Tes t s 7 -9
7 .5 .1 Po ros i t y Tes t Resu l t s 7 -9
7 .5 .2 Oxygen Pe rmeab i l i t y Tes t Resu l t s 7 -11
7 .6 Conc lus i on 7 -12
8 . CON CLU SIONS A ND RE CO MMENDATIONS 8 -1
8 . 1 Conc lus i ons 8 -1
8 .2 Recomme nda t i ons 8 -3
9 . REFER E NCES 9 -1
APPENDI X A Cumu la t i ve Pa r t i c l e S i ze D i s t r i bu t i on o f Gas i f i ca t i on
Ash , Cemen t and Gas i f i ca t i on Ash and Ceme n t
I n t e rg round and I n te rb l ended
APPENDI X B Cumu la t i ve % Ove rs i ze Pa r t i c l e S i ze D i s t r i bu t i on f o r
Gas i f i ca t i on Ash , Cemen t a nd Gas i f i ca t i on Ash and
Cemen t I n t e rg round and I n te rb l ended
APPENDI X C Ros in -Rammle r D i s t r i bu t i on G raphs
APPENDI X D B la i ne Su r f ace A rea Ca l cu l a t i ons
APPENDI X E Mor ta r P r i sms S t reng th Summary f o r t he E f f ec t o f
G r i nd i ng T ime on t he P rope r t i es o f I n t e rb l ended
Gas i f i ca t i on Ash and Ceme n t
APPENDI X F Mor ta r P r i sms S t reng th Summary f o r t he E f f ec t o f
G r i nd i ng T ime on t he P rope r t i es o f I n t e rg round
Gas i f i ca t i on Ash and Ceme n t
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
APPENDI X G Mor ta r P r i sms S t reng th Summary f o r t he E f f ec t o f
Gypsu m Con ten t on t he P rope r t i es o f I n t e rg round
Gas i f i ca t i on Ash and Ceme n t
APPENDI X H Mo r ta r P r i sms S t reng th Summary f o r t he E f f ec t o f
Rep lacemen t Leve l s on t he P rope r t i es o f I n te rg round
Gas i f i ca t i on Ash and Ceme n t
APPENDI X I Mo r ta r P r i sms S t reng th summary f o r t he Comp ar i son
be tween Manu fac tu red and Commerc i a l Cemen t
APPENDI X J Cube S t reng th Summar y
APPENDI X K Spec i f i c C reep Summar y
APPENDI X L Po ros i t y Summary
APPENDI X M Pe rmeab i l i t y Ca l cu la t i ons
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
LIST OF F IGURES PAGE
F i gu re 2 .1 Cemen t manu fac tu re and t he i n f l uenced aspec t s
( f r om ww w.wbcsdcemen t . o rg , 2005 ) 2 -3
F i gu re 2 .2 Changes i n Ca 2 + i n so l u t i on cu r i ng C 3 S hyd ra t i on vs .
t ime i n t he absence and p resence o f gypsum
(F r i g i one , 1995 ) 2 -7
F i gu re 2 .3 Op t im i za t i on o f so l ub le ca l c i um su lpha te ( cemen ts )
(Newman , 2003 ) 2 -9
F i gu re 2 .4 Exa mp le o f no rma l hyd ra t i on o f Po r t l and cemen t
(Sandbe rg , 2004 ) 2 -11
F igu re 2 .5 D iag rammat i c r ep resen ta t i on o f Ros in -Ramle r
d i s t r i bu t i on f unc t i on (Wa in r i gh t and O lo runsogo ,
1999 ) 2 -15
F i gu re 3 .1 Coa l combus t i on by -p roduc t s 3 -4
F i gu re 3 .2 A mode rn pu l ve r i sed coa l - f i r ed t he rma l power s t a t i on
( f r om So u th A f r i can Coa l Ash Assoc ia t i on , 1999 ) 3 -6
F i gu re 3 .3 E l ec t r on m i c roscope pho tog raph o f f l y ash . 3 -7
F i gu re 3 .4 Re la t i onsh ip be tween wa te r r equ i r emen t and cemen t
r ep l acemen t w i t h f l y ash (Na i k , 1990 ) 3 -11
F igu re 3 .5 Deve lop men t o f compress i ve s t r eng ths o f Po r t l and
cemen t and f l y ash conc re tes ( f r om Sou th A f r i can
Coa l Ash Assoc ia t i on , 1999 ) 3 -13
F igu re 3 .6 E f f ec t o f coa rse f rac t i ons o f f l y ash on compress i ve
s t r eng th deve lopmen t o f conc re tes ( Josh i , 1982 ) 3 -14
F igu re 3 .7 Compres s i ve s t r eng ths o f PC and PC /30FA a t d i f f e ren t
t empe ra tu res (Sou th A f r i can Coa l Ash Assoc ia t i on ,
1999 ) 3 -15
F i gu re 3 .8 The i n f l uence o f FA con ten t o f t he cemen t i t i ous
ma te r i a l on t he f l exu ra l / compress i ve s t r eng th r a t i o o f
conc re te ( f r om So u th A f r i can Coa l Ash Assoc ia t i on ,
1999 ) 3 -16
F i gu re 3 .9 The i n f l uence o f FA on t he e l as t i c modu lus / compress i ve
s t r eng th o f conc re te ( f r om Sou th A f r i can Coa l Ash
Assoc ia t i on , 1999 ) 3 -17
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
F igu re 3 .10 D ry i ng sh r i nkage o f conc re te i nco rpo ra t i ng f l y ash
(Yuan , 1983 ) 3 -18
F i gu re 4 .1 Labo ra to r y ba l l m i l l u sed i n expe r ime n t 4 -2
F i gu re 4 .2 S tee l ba l l s used f o r g r i nd i ng 4 -2
F i gu re 4 .3 Cumu la t i ve pa r t i c l e s i ze o f s t ee l ba l l s 4 -3
F i gu re 4 .4 Samp le o f gas i f i ca t i on ash c l i n ke r 4 -4
F i gu re 4 .5 Exponen t i a l f i t f o r cumu la t i ve % ove rs i ze pa r t i c l e
s i ze d i s t r i bu t i on 4 -5
F i gu re 4 .6 Ros in -Rammle r d i s t r i bu t i on g raph 4 -6
F i gu re 4 .7 Exp lana t i on o f Ros in -Rammle r d i s t r i bu t i on pa rame te r s 4 -6
F i gu re 4 .8 Cumu la t i ve % ove rs i ze d i s t r i bu t i on pa rame te r s 4 -7
F i gu re 4 .9 Cumu la t i ve % ove rs i ze i n t e r va l s f o r 3µm and 30µm 4 -8
F i gu re 4 .10 Appa ra tus t o de te rm ine spec i f i c su r face a rea 4 -9
F i gu re 4 .11 Pho to o f samp le on f l ow t ab le a f t e r mou ld i s r emoved 4 -14
F igu re 4 .12 Pho to o f d i ame te r measu remen ts o f f l ow t ab le t es t 4 -15
F igu re 4 .13 Pho to o f mou ld used 4 -15
F igu re 4 .14 Le Cha te l i e r mou lds i n hum id i t y cab ine t 4 -17
F i gu re 5 .1 Measu r i ng t he s l ump (Add i s , 2001 ) 5 -3
F i gu re 5 .2 Pho to o f l ab se t - up f o r measu r i ng sh r i nkage and
C reep 5 -7
F i gu re 5 .3 Pho to o f po ros i t y t es t se t up 5 -9
F i gu re 6 .1 G raph o f cumu la t i ve pa r t i c l e s i ze d i s t r i bu t i on o f
cemen t and gas i f i ca t i on ash (g r i nded sepa ra te and
i n t e rg round ) 6 -2
F i gu re 6 .2 Cumu la t i ve pa r t i c l e s i zes fo r gas i f i ca t i on ash and
cemen t i n t e rg round 6 -3
F i gu re 6 .3 Summary o f exponen t i a l f i t t ed f unc t i ons f o r t he
cumu la t i ve % ove rs i ze pa r t i c l e s i ze d i s t r i bu t i on 6 -3
F i gu re 6 .4 Summary o f Ros in -Rammle r d i s t r i bu t i ons 6 -4
F i gu re 6 .5 Re la t i on be tween g r i nd i ng t ime and pos i t i on
pa rame te r X o 6 - 7
F i gu re 6 .6 Re la t i onsh ip be tween g r i nd i ng t ime and s l ope
pa rame te r ( n ) 6 -8
F i gu re 6 .7 Scann ing e l ec t r on m i c roscope pho to o f f l y ash 6 -10
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
F igu re 6 .8 Scann ing e l ec t r on m i c roscope pho to o f gas i f i ca t i on
a sh 6 -11
F i gu re 6 .9 G raph i nd i ca t i ng B la i ne su r f ace a rea 6 -11
F i gu re 6 .10 XRD resu l t s f o r gas i f i ca t i on ash 6 -14
F igu re 6 .11 Compres s i ve s t r eng ths f o r i n t e rb l end ing gas i f i ca t i on
ash and cemen t 6 -16
F igu re 6 .12 F l exu ra l s t r eng ths f o r i n t e rb l end ing gas i f i ca t i on ash
and cemen t 6 -18
F igu re 6 .13 Re la t i on be tween compress i ve s t r eng ths and
Ros in -Rammle r d i s t r i bu t i on pos i t i on pa rame te r (X o )
f o r i n t e rb l end ing gas i f i ca t i on ash and cemen t 6 -19
F i gu re 6 .14 Re la t i on be tween compress ion s t r eng ths and
Ros in -Rammle r d i s t r i bu t i on s l ope (n ) pa rame te r f o r
i n t e rb l end ing gas i f i ca t i on ash and cemen t 6 -20
F i gu re 6 .15 Re la t i on be tween compress ion s t r eng th and pa r t i c l e
s i ze d i s t r i bu t i on pa rame te r s f o r i n t e rb l end ing
gas i f i ca t i on ash and cemen t 6 -21
F igu re 6 .16 Compres s i ve S t reng th f o r i n t e rg r i nd i ng gas i f i ca t i on
ash and cemen t 6 -22
F igu re 6 .17 F l exu ra l s t r eng ths f o r i n t e rg r i nd i ng gas i f i ca t i on ash
and cemen t 6 -24
F igu re 6 .18 Re la t i on compress i ve s t r eng ths and Ros in -Rammle r
d i s t r i bu t i on pos i t i on pa rame te r (X o ) f o r i n t e rg r i nd i ng
gas i f i ca t i on ash and cemen t 6 -25
F igu re 6 .19 Re la t i on be tween 28 -day compress ion s t r eng ths and
Ros in -Rammle r d i s t r i bu t i on s l ope (n ) pa rame te r 6 -26
F igu re 6 .20 Re la t i on be tween 28 -day compress ion s t r eng th and
pa r t i c l e s i ze d i s t r i bu t i on pa rame te r s 6 -27
F igu re 6 .21 Compres s i ve s t r eng ths f o r gypsum con ten t 6 -28
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
F igu re 6 .22 F l exu ra l s t r eng ths f o r gypsum con ten t 6 -29
F igu re 6 .23 Ra te o f hea t deve lopmen t f o r d i f f e ren t gypsum
pe r cen tages 6 -30
F igu re 6 .24 The d i f f e rence i n t he r a te o f hea t evo lu t i on f o r
d i f f e ren t gypsum p e rcen tages cemen t and pu re PC
cemen t 6 -31
F igu re 6 .25 To ta l hea t o f hyd ra t i on o f d i f f e ren t gypsum pe rcen tage
cemen ts a t 25 ºC 6 -32
F igu re 6 .26 Compres s i ve s t r eng th f o r d i f f e ren t r ep lacemen t
l e ve l s o f gas i f i ca t i on ash 6 -33
F igu re 6 .27 F l exu ra l s t r eng ths f o r d i f f e ren t r ep lac emen t l eve l s o f
gas i f i ca t i on ash 6 -34
F igu re 6 .28 Re la t i on compress i ve s t r eng ths and Ros in -Rammle r
d i s t r i bu t i on pos i t i on pa rame te r (X o ) f o r r ep lacemen t
l e ve l s o f gas i f i ca t i on ash 6 -36
F igu re 6 .29 Re la t i on be tween 28 -day compress ion s t r eng ths and
Ros in -Rammle r d i s t r i bu t i on s l ope (n ) pa rame te r 6 -36
F igu re 6 .30 Re la t i on be tween 28 -day compress ion s t r eng th and
pa r t i c l e s i ze d i s t r i bu t i on pa rame te r s o f r ep l acemen t
l e ve l o f gas i f i ca t i on ash 6 -37
F igu re 6 .31 Compres s i ve s t r eng ths f o r manu fac tu red and
commerc i a l l y ava i l ab l e cemen t 6 -38
F igu re 6 .32 F l exu ra l s t r eng ths f o r manu fac tu red and
commerc i a l l y ava i l ab l e cemen t 6 -40
F igu re 6 .33 Ra te o f hea t deve lopmen t f o r manu fac tu red and
commerc i a l l y ava i l ab l e cemen t 6 -41
F i gu re 7 .1 S l ump t es t f o r conc re te m i xes 7 -2
F i gu re 7 .2 Conc re te cubes compress i on s t r eng th r esu l t s 7 -3
F i gu re 7 .3 Tens i l e s t r eng th r esu l t s f o r conc re te m i xes 7 -4
F i gu re 7 .4 E -va lue t es t r esu l t s f o r conc re te m i xes 7 -5
F i gu re 7 .5 Sh r i nkage and c reep resu l t s f o r i n t e rg round
gas i f i ca t i on ash m ix 7 -7
F i gu re 7 .6 Sh r i nkage and c reep resu l t s f o r i n t e rb l ended f l y
a sh m i x 7 -8
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
F igu re 7 .7 Sh r i nkage and c reep resu l t s f o r i n t e rb l ended
gas i f i ca t i on ash m ix 7 -8
F i gu re 7 .8 Spec i f i c c reep resu l t s f o r t he t h ree d i f f e ren t m i xes 7 -9
F i gu re 7 .7 Po ros i t y r esu l t s o f conc re te m i xes 7 -10
F igu re 7 .8 Oxygen p e rmeab i l i t y t es t r esu l t s f o r conc re te m i xes 7 -11
F igu re 7 .9 Oxygen p e rmeab i l i t y i ndex resu l t s f o r t he conc re te
m i xes 7 -12
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
LIST OF TABLES PAGE
Tab le 2 .1 Common Po r t l and and Po r t l and f l y ash cemen ts
( f r om SANS 50197 -1 /SABS EN 197 -1 :20001 ) 2 -4
Tab le 2 .2 Mechan i ca l and Phys i ca l r equ i r emen ts o f cemen t
( f r om SANS 50197 -1 /SABS EN 197 -1 :2000 ) 2 -5
Tab le 3 .1 Typ i ca l chem ica l compos i t i on o f f l y ash (Add i s , 2001 ) 3 -8
Tab le 3 .2 Chem ica l spec i f i ca t i ons fo r cemen t ex tende rs .
(SANS 1491 -2 :2005 / SABS 194 1 -2 :2005 ) 3 -9
Tab le 4 .1 M i x compos i t i on f o r mo r ta r p r i sms 4 -13
Tab le 4 .8 M i x compos i t i on used i n t es t 4 -13
Tab le 4 .3 Mo r ta r p r i sm m ix compos i t i on f o r i n t e rb l end ing cemen t
and Gas i f i ca t i on ash 4 -19
Tab le 4 .2 Mo r ta r p r i sm m ix compos i t i on f o r i n t e rg r i nd i ng cemen t
and Gas i f i ca t i on ash 4 -19
Tab le 4 .5 Gypsu m rep lacemen t we igh t s f o r mo r ta r p r i sms 4 -19
Tab le 5 .1 M i x compos i t i on f o r conc re te m i xes 5 -2
Tab le 5 .2 Conc re te m i x compos i t i on 5 -2
Tab le 6 .1 F i t t ed func t i ons o f ove rs i ze pa r t i c l e s i ze d i s t r i bu t i on 6 -5
Tab le 6 .2 Ros in -Rammle r pa r t i c l e s i ze d i s t r i bu t i on pa rame te r s 6 -6
Tab le 6 .3 Ove rs i ze pa r t i c l e s i ze d i s t r i bu t i on pa rame te r s 6 -9
Tab le 6 .4 XRF re su l t s 6 -13
Tab le 6 .5 Chem ica l t es t r esu l t s 6 -15
Tab le 6 .6 S t r eng th c l asses o f i n t e rb l end ing m ixes g r i nd i ng t ime 6 -17
Tab le 6 .7 Pe rcen tage o f compress i ve s t r eng th ach ieved f o r
i n t e rb l end ing 6 -18
Tab le 6 .8 S t r eng th c l asses f o r i n t e rg r i nd i ng m ixes g r i nd i ng t ime 6 -23
Tab le 6 .9 Pe rcen tage o f compress i ve s t r eng th ach ieved f o r
i n t e rg r i nd i ng 6 -24
Tab le 6 .10 S t r eng th c l asses f o r d i f f e ren t r ep l acemen t l eve l s o f
gas i f i ca t i on ash 6 -34
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
Tab le 6 .11 Pe rcen tage o f compress i ve s t r eng th ach ieved f o r d i f f e ren t
r ep l acemen t l eve l s o f gas i f i ca t i on ash 6 -35
Tab le 6 .12 S t r eng th c l asses f o r d i f f e ren t r ep l acemen t l eve l s o f
gas i f i ca t i on ash 6 -39
Tab le 6 .13 Pe rcen tage o f compress i ve s t r eng th ach ieved f o r d i f f e ren t
r ep l acemen t l eve l s o f gas i f i ca t i on ash 6 -40
Tab le 7 .1 Tab le compa r i ng t ens i l e and compress i ve s t r eng ths 7 -4
Tab le 7 .2 E - va lue resu l t s o f t he d i f f e ren t cy l i nde rs f o r t he
d i f f e ren t m i xes 7 -6
Tab le 7 .3 Sh r i nkage , C reep and Spec i f i c C reep Resu l t s f o r t he
d i f f e ren t m i xes 7 -6
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
1-1
1 . INTRODUCTION 1 .1 BAC KGR OUN D
I n r ecen t yea rs t he re has been a s i gn i f i can t i nc rease i n t he use
o f was te ma te r i a l s as bo th cemen t ex tende rs and f i l l e r s i n
conc re te (Esca lan te , 2004 ) . The reason f o r t h i s i s a g row ing
awa reness o f t he eng inee r i ng , ec onom ica l and ec o log i ca l
bene f i t s , t he use o f was te ma te r i a l s have i n t he cemen t and
conc re te i ndus t r i es . Was te ma te r i a l s can howeve r on l y be used
i n conc re te i f t hey a re no t de t r imen ta l t o t he sho r t - o r t he l ong -
t e rm p rope r t i es o f t he conc re te .
The ma in r eason f o r t he use o f ex te nde rs i n conc re te i s t he i r
va r i e t y o f use fu l enhancemen ts o f o r mod i f i ca t i ons t o t he
conc re te p rope r t i es . Cemen t ex t ende rs have two common
f ea tu res :
• t he i r pa r t i c l e s i ze r ange i s s im i l a r t o o r sma l l e r t han tha t
o f Po r t l and cemen t .
• t hey become i nvo l ved i n t he hyd ra t i on r eac t i ons .
I n b l ended cemen t p roduc t i on , ex tende rs can be i n t r oduced t o
t he cemen t by i n t e rb l end ing o r i n t e rg r i nd i ng (E rdogdu , 1999 ) .
The f eed t o Saso l gas i f i e r s p r i nc i pa l l y cons i s t s o f coa rse coa l
( >5mm) and ex t r aneous rock f r agmen ts ( s t one ) . Du r i ng t he
gas i f i ca t i on o f t h i s coa rse coa l a t e l eva ted t empe ra tu res and
p ressu re a m i x tu re o f ca rbon monox ide and hyd rogen (a l so
r e fe r red t o as syn thes i s gas ) i s p roduced . The coa rse ash i s
f o rmed a t t hese e l eva ted t empe ra tu res and p ressu re by t he
i n t e rac t i on o f i ne r t m ine ra l s p resen t i n t he coa l and s tone . The
coa rse ash i s r emoved f r o m the ga s i f i e r and d i sposed as a by -
p roduc t (Van Dyk , 2005 ) .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
1-2
1 .2 OBJE CTI VES OF THE STUDY
The ma in a im o f t h i s i nves t i ga t i on i s t o de te rm ine t he
su i t ab i l i t y o f us i ng gas i f i ca t i on as h as cemen t e x tende r i n
conc re te . To mee t t h i s a im , t he ob jec t i ves o f t he i nves t i ga t i on
a re as f o l l ows :
• To i nves t i ga te t he p rope r t i es o f cemen t ma nu fac tu r i ng w i t h
spec i f i c re f e rence t o cemen t c l asses , hyd ra t i on o f cemen t ,
and t he op t im i sa t i on o f gypsum, spec i f i c su r f ace a rea and
pa r t i c l e s i ze d i s t r i bu t i on , t o eva lua te t he pe r f o rma nce o f
cemen t p roduced i n t he l abo ra to r y .
• I nves t i ga te t he phys i ca l , chemica l and m ine ra l og i ca l
compos i t i on o f a gas i f i ca t i on ash samp le t o de te rm ine i f
gas i f i ca t i on ash can be used as a ceme n t ex ten de r i n
conc re te .
• De te rm in e t he comp l i ance o f gas i f i ca t i on ash w i t h t he
r equ i r emen ts f o r us e i n cemen t .
• De te rm in e an op t imum g r i nd ing t ime f o r bo th t he
i n t e rb l end ing and i n t e rg r i nd i ng o f gas i f i ca t i on ash and
cemen t .
• De te rm in e t he e f fec t o f r ep l acemen t l eve l on t he p rope r t i es
o f i n t e rb l ended and i n t e rg round gas i f i ca t i on as h and cemen t .
• I n ves t i ga te t he e f f ec t o f i n t e rb l ended and i n t e rg round
gas i f i ca t i on ash and cemen t on t he sho r t and l ong t e rm
p rope r t i es o f conc re te .
• I n ves t i ga te t he e f f ec t o f t he gas i f i ca t i on ash on t he
du rab i l i t y o f conc re te .
1 .3 SCOPE OF THE ST UDY
Th i s s tudy w i l l cons i s t o f a l i t e ra tu re r ev i ew on t he manu fac tu re
and p rope r t i es o f cemen t . De ta i l o f d i f f e ren t coa l ash by -
p roduc t s i s d i s cussed and t he use o f f l y a sh as a cemen t
ex tende r i n conc re te i s cons ide red . Cons ide ra t i on i s g i ven t o
p rope r t i es l i ke m ine ra l og i ca l and chem ica l compos i t i on , shape ,
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
1-3
pa r t i c l e s i ze d i s t r i bu t i ons , chem ica l r equ i r emen ts o f us i ng f l y
ash i n conc re te , s t r eng th deve lopmen t a nd du rab i l i t y o f
conc re te .
A gas i f i ca t i on ash samp le i s t es ted to de te rm ine how th i s was te
ma te r i a l compa res t o t he ex tende rs cu r ren t l y used i n t he
cemen t i ndus t r y . Cons ide ra t i on i s g i ven t o t he chem ica l and
phys i ca l p rope r t i es o f gas i f i ca t i on as h . A l l da ta i s ana l ysed t o
ach ieve conc lus i ons on t he above -me n t i oned ob jec t i ves .
Cemen t i s manu fac tu red by g r i nd i ng c l i nke r . Pa r t i c l e s i ze
d i s t r i bu t i ons a re i nves t i ga ted and op t imum g r i nd i ng t imes i s
i nves t i ga ted . The op t im i sa t i on o f gypsum i s a l so i nves t i ga ted
w i t h r e fe rence t o t he hyd ra t i on o f cemen t . D i f f e ren t
r ep l acemen t l eve l s o f gas i f i ca t i on ash a re i nves t i ga ted t o
de te rm ine res t r i c t i on on t he use o f gas i f i ca t i on ash i n cemen t .
Gas i f i ca t i on ash i s used i n conc re te and t he s t r eng th
deve lopmen t , de fo rma t i on and du rab i l i t y o f t hese conc re te
m i xes a re exam in ed . Th i s w i l l p rov i de adequa te unde rs tand ing
o f t he advan tages t ha t was te ma te r i a l s have t o bo th t he cemen t
i ndus t r y and t he env i r onme n t .
To accu ra te l y es t ima te and p red i c t behav iou r , i t i s necessa ry t o
r epea t t es t s on as many i n dependen t samp les as poss ib l e . I n
t h i s s t udy t he t es t s we re o n l y conduc ted once . The re fo re i t i s
no t s t a t i s t i ca l l y co r rec t t o d raw f i na l conc lus i ons and p red i c t
t r ends based on t he r esu l t s .
Th i s s t udy does no t i n c l ude t he f o l l ow ing :
• The e f f ec t o f va r i ab i l i t y o f gas i f i ca t i on ash as f a r as
phys i ca l and chem ica l p rope r t i es i s conce rned .
• The response o f gas i f i ca t i on ash t o adm ix tu res .
• The e f f ec t o f gas i f i ca t i on as h on t he l ong - t e rm du rab i l i t y
o f conc re te .
• Du rab i l i t y t es t s pe r f o rmed exc l udes t he dama g ing e f f ec t s
o f u l t r a v i o l e t (UV) l i gh t and phys i ca l s cou r i ng .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
1-4
1 .4 METHODOLOGY
The re we re seven p r i nc i pa l ob j ec t i ves i n t h i s r esea rch p ro j ec t .
The me t hodo logy f o l l owed i n each i s se l ec ted t o ob jec t i ve l y
eva lua te gas i f i ca t i on ash f o r i t s use i n cemen t and conc re te .
• The phys i ca l p rope r t i es o f a gas i f i ca t i on ash samp le w i l l
be i nves t i ga ted by exam in i ng t he pa r t i c l e s i ze d i s t r i bu t i on
and shape . Th i s i nc l udes de te rm in i ng an op t imu m
g r i nd i ng t ime and gypsum con ten t .
• The chemica l and m ine ra l og i ca l compos i t i on o f a
gas i f i ca t i on ash samp le i s i nves t i ga ted and compa red t o
t ha t o f ex tende rs commo n l y used t ha t a re known t o
enhance t he p rope r t i es o f conc re te .
• The comp l i ance o f a gas i f i ca t i on ash w i t h t he chem ica l
r equ i r emen ts f o r us e i n conc re te i s de te rm ined .
• The reac t i v i t y o f gas i f i ca t i on ash i s es tab l i shed by
cons ide r i ng i n t e rb l end ing and i n t e rg r i nd i ng i n mo r ta r , and
t es t i ng aga ins t f l y ash i n conc re te .
• The e f f ec t o f gas i f i ca t i on as h on t he sho r t and l ong t e rm
p rope r t i es o f conc re te i s es tab l i shed by measu r i ng
wo rkab i l i t y , s t r eng th deve lopmen t , e l as t i c i t y , sh r i nkage
and c reep , po ros i t y and pe rmeab i l i t y .
• I n conc lus i on recommenda t i ons a re made f o r t he use o f
gas i f i ca t i on ash .
1 .5 ORGANI SAT ION OF THE REPORT
The d i sse r t a t i on has been d i v i ded i n t o t he f o l l ow ing sec t i ons :
• Chap te r 1 se r ves as an i n t roduc t i on t o t he t hes i s .
• Po r t l and cemen t as we l l as p rope r t i es o f manu fac tu r i ng o f
cemen t i s d i s cussed i n chap te r 2 .
• The compos i t i on and p rope r t i es o f coa l ash a re d i scussed i n
Chap te r 3 , w i t h spec ia l r e fe rence t o t he p rope r t i es o f f l y ash .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
1-5
• Chap te r 4 desc r i bes t he expe r imen ta l p rog ramme an d t es t
p rocedu res f o r cemen t .
• Expe r ime n ta l p rog ramme a nd t es t p rocedu res f o r conc re te
a re d i scussed i n Chap te r 5 .
• Chap te r 6 con ta i ns t he r esu l t s f o r t he p rope r t i es and
u t i l i sa t i on o f gas i f i ca t i on as h as a r ep l acemen t o f cemen t i n
mo r ta r p r i sms .
• The resu l t s o f us i ng gas i f i ca t i on ash as a cemen t ex tende r
i n conc re te a re eva lua ted i n Chap te r 7 .
• Chap te r 8 con ta i ns t he conc lus i ons and recommenda t i ons o f
t he s t udy .
• A l i s t o f re f e rences f o l l ows i n Chap te r 9 .
• Va r i ous r esu l t s a re p rov i ded i n t he append i ces . These
append i ces a re r e fe r red t o i n t he ma i n body o f t he
d i sse r t a t i on .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
2-1
2. COMPONENTS AND PROPERTIES OF PORTLAND CEMENT
2 .1 INTRODUCTION
Globa l popu la t i on i s r i s i ng , p l ac i ng i nc reas ing p ressu re on
essen t i a l na tu ra l r esou rces such as l and and ene rgy . Th i s
makes i t impe ra t i ve f o r us t o f i nd ways o f us i ng t hese
resou rces mo re e f f i c i en t l y . Th i s need f o r mo re env i r onmen ta l l y
and soc ia l l y sus ta i nab le deve lopmen t has become a key
agenda f o r gove rnmen ts , non -gove rnmen ta l o rgan i sa t i ons
(NGO) an d bus inesses .
Cemen t i s an essen t i a l ma te r i a l i n t oday ' s soc i e t y because , as
a ma jo r cons t i t uen t o f conc re te , i t f o rms a f undamen ta l e l emen t
o f any hous ing o r i n f r as t ruc tu re deve lopme n t . The chem ica l
p rocess o f mak ing cemen t c l i nke r p roduces CO 2 , a ma jo r
g reenhouse gas con t r i bu t i ng t o c l ima te change .
I n t h i s chap te r , de ta i l o f t he manu fa c tu r i ng o f Po r t l and cemen t
(PC) , cemen t c l asses and t he hyd ra t i on o f cemen t w i l l be
d i scussed . Cons ide ra t i on w i l l be g i ven t o p rope r t i es l i ke t he
op t im i sa t i on o f su l pha te and f i neness o f cemen t . The pa r t i c l e
s i ze d i s t r i bu t i on i s d i s cussed w i t h spec i f i c r e f e rence t o t he
Ros in -Rammle r d i s t r i bu t i on f unc t i on . Th i s w i l l p rov i de adequa te
unde rs tand ing o f t he p rope r t i es o f cemen t and t he i n f l uence
b l ended cemen ts have on t he cemen t hyd ra t i on p rocess .
2 .2 CEMENT MAN UFA CTURE
SANS 50 197 -1 /SABS EN 1 97 -1 :2000 s ta tes t ha t “ cemen t i s a
hyd rau l i c b i nde r , a f i ne l y g round i no rgan i c ma te r i a l wh i ch ,
when m ixed w i t h wa te r , f o rms a pas te wh i ch se t s and ha rdens
by means o f hyd ra t i on r eac t i ons and p rocesses and wh i ch a f t e r
ha rden ing , r e ta i ns i t s s t r eng th and s tab i l i t y even unde r wa te r . ”
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
2-2
Cemen t i s manu fac tu red f rom fou r r aw ma te r i a l ox i des : l ime ,
s i l i ca , a lum ina and f e r r i c ox i de . L ime canno t be f ound i n na tu re
and i s p roduced by hea t i ng ca l c i um ca rbona te (Add i s , 2001 ) .
Cemen t manu fac tu r i ng cons i s t s o f qua r r y i ng o r excava t i ng r aw
ma te r i a l s . Cemen t manu fa c tu re r s ob ta i n s i l i ca , a l um ina and
f e r r i c ox i des f r om c l ay o r sha le . The raw ma t e r i a l s a re c rushed ,
b l ended , m i l l ed and p rehea ted i n a k i l n . I n t he k i l n , ca l c i um
ca rbona te i s conve r t ed t o ca l c i um ox ide a t t empe ra tu res o f
800°C t o 1000°C :
CaCO 3 → CaO + CO 2 ( equa t i on 2 .1 )
The ma te r i a l s f l ow t o a ho t te r ( 1450°C) pa r t o f t he k i l n whe re ,
t he b l end o f t he f ou r ox i des i s conve r t ed t o cemen t c l i n ke r
(Add i s , 2001 ) . The c l i nke r i s t hen g round w i t h a sma l l amoun t
o f gypsum i n to a powde r w i t h a spec i f i c su r face a rea (B la i ne )
o f 300 – 350 m² / k g t o ma ke ‘O rd ina ry Po r t l and Cemen t ’ , t he
mos t common l y used t ype o f cemen t ( o f t en re fe r red t o as
OPC) . A schema t i c p resen ta t i on o f t he cemen t manu f ac tu r i ng
p rocess can be seen i n F i gu re 2 .1 .
The CO 2 em iss i ons f r om Po r t l and cemen t manu fac tu r i ng a re
gene ra ted by two mechan i sms . These mechan i sms a re t he
ca l c i n i ng o f l imes tone ( see equa t i on 2 .1 ) and t he comb us t i on o f
f ue l s t o gene ra te ene rgy . Typ i ca l l y , Po r t l and cemen t con ta i ns
t he equ i va l en t o f abou t 63 .5 % CaO. Consequen t l y , abou t 1 .135
un i t s o f CaCO 3 a re r equ i r ed t o p roduce 1 un i t o f cemen t , and
t he amoun t o f CO 2 r e l eased i n t he ca l c i n i ng p rocess i s abou t
500 k i l og rams ( kg ) pe r me t r i c t on o f Po r t l and cemen t p roduced
(1 ,000 pounds [ l b ] pe r t on o f cemen t ) . To ta l CO 2 em iss i ons
depend on ene rgy consump t i on and gene ra l l y f a l l i n t he r ange
o f 0 . 85 to 1 .35 me t r i c t on o f CO 2 pe r me t r i c t on o f c l i n ke r
(www. wb csdcemen t . o rg , 2005 ) . Th i s means t ha t t he cemen t
i ndus t r y p roduces 5% o f g l oba l man -made CO 2 e m iss i ons , o f
wh i ch 50% i s f r om the chemica l p rocess , and 40% f r om bu rn i ng
f ue l . The rema inde r i s sp l i t be tween e l ec t r i c i t y and t r anspo r t
us es . C l ima te p ro tec t i on , and i n pa r t i c u l a r r educ t i on o f c a rbon
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
2-3
d iox i de (CO 2 ) e m iss i ons i s t he re fo re an i s sue wh i ch ve r y
se r i ous l y needs t o be add ressed by t he cemen t i ndus t r y .
F i gu re 2 .1 Cemen t manu fac tu re and t he i n f l uenced aspec t s
( f r om ww w.wbcsdcemen t . o rg , 2005 )
Because c l ima te p ro tec t i on has such a h i gh p ro f i l e i n t he
i ndus t r y , e f f ec t i ve s t r a teg ies f o r manag ing CO 2 e m iss i ons a re
o f c ruc i a l impo r t ance i n t he ma rke tp l ace . The reduc t i on
op t i ons a re l i ke l y t o i nc l ude : i nnova t i on i n imp rov ing t he
ene rgy e f f i c i ency o f p rocesses and equ ipmen t ; sw i t ch i ng to
l owe r ca rbon f ue l s ; us i ng a l t e rna t i ve r aw ma t e r i a l s t o r educe
l imes tone use ; deve lop ing CO 2 cap tu re and seques t ra t i on
t echn iques ; and t ak i ng advan tage o f ma rke t mechan i sms such
as em iss i ons t r ad ing and vo lun ta r y i n i t i a t i ves .
The use o f was te ma te r i a l s dec rease t he amoun t o f c l i n ke r
manu fac tu red and t hus dec reases t he amoun t o f CO 2
em iss i ons .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
2-4
2 .3 CEMENT CLASSES
Tab le 2 .1 i nd i ca tes t he mo s t commo n Po r t l and and Po r t l and f l y
ash cemen t used i n Sou th A f r i ca . Tab le 2 .2 i nd i ca tes t he
mechan i ca l and phys i ca l r equ i r emen ts o f cemen t used i n Sou th
A f r i ca . These t ab l es a re used t o desc r i be t he commerc i a l l y
ava i l ab l e cemen t . The c l ass i f i ca t i on o f cemen ts i n t e rms o f
t he i r s t r eng th -g i v i ng p rope r t i es has been p rac t i sed fo r many
yea rs .
Tab le 2 .1 Common Po r t l and and Po r t l and f l y as h cemen ts ( f r om SANS
50197 -1 /SABS EN 197 -1 :2000 )
Composition (percentage by mass)
Main constituents
Pozzolana Fly ash
clinker natural natural
calcined siliceous calcer
ous
Minor additio
nal constituents Main
types Notation of the
products K P Q V W
CEM I Portland cement CEM I 95-100 - - - - 0-5
CEM II/A-V 80-94 - - 6-20 - 0-5
CEM II/B-V 65-79 - - 21-35 - 0-5
CEM II/A-W 80-94 - - - 6-20 0-5
CEM II
Portland fly ash cement CEM II/B-W 65-79 - - - 21-35 0-5
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
2-5
Tab le 2 .2 Mechan i ca l and Phys i ca l requ i r emen ts o f cemen t ( f r om SANS
50197 -1 /SABS EN 197 -1 :2000 )
Compressive strength MPa
Early Strength Standard Strength Strength
Class 2 Days 7 Days 28 Days
Initial setting
time
Soundness (expansion)
mm
32.5 N - ≥16.0
32.5 R ≥ 10.0 - ≥ 32.5 ≤ 52.5 ≥ 75
42.5 N ≥ 10.0 -
42.5 R ≥ 20.0 - ≥ 42.5 ≤ 62.5 ≥ 60
52.5 N ≥ 20.0 -
52.5 R ≥ 30.0 - ≥ 52.5 - ≥ 45 ≤ 10
2 . 4 HYDR ATI ON OF P ORTLA N D CE MEN T
The se t t i ng and ha rden ing o f Po r t l and cemen t occu r as a r esu l t
o f t he r e ac t i on be tween t h e compo unds o f cemen t a nd wa te r .
The ma jo r compounds o f cemen t t ha t r eac t w i t h wa te r t o
p roduce reac t i on p roduc t s a re t r i ca l c i um s i l i ca te (C 3 S ) ,
d i ca l c i um s i l i ca te (C 2 S ) , t r i ca l c i um a lum ina te (C 3 A ) , and
t e t r aca l c i um a lum i no fe r r i t e (C 4 AF ) (Nev i l l e , 1995 ) .
The p resence o f gypsum a f f ec t s t he hyd ra t i on pa t te rn o f PC
bo th k i ne t i ca l l y and t he rmo dynam ica l l y . F i r s t l y t he i n f l uence o f
gypsum on t he p r i nc i pa l i nd i v i dua l cons t i t uen t s i s d i s cussed
and t hen t he i n f l uence o f t he r eac t i ons as a who le wh i ch occu r
w i t h PC hyd ra t i on .
2 .4 .1 The h ydra t ion o f C 3 S and C 2 S
The ha rden ing o f cemen t pas te i s due ma in l y t o t he f o rma t i on
o f Ca l c i um s i l i ca te hyd ra te (CSH) , and t h i s f o rma t i on i s
a f f ec ted by t he p resence o f CaSO 4 i n t he pas te . The g ypsum i n
cemen t no t on l y a f f ec t s t he se t t i ng t ime , bu t a l so t he s t r eng th
deve lopmen t . The op t imum gypsu m con ten t i s t he va lue a t
wh i ch t he op t imum comb ina t i on o f quan t i t y and qua l i t y occu rs .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
2-6
Loche r e t a l ( 1995 ) , have d i scussed f ac to r s gove rn i ng t he
op t imum gypsum con ten t and t he e f fec t s o f va r y i ng t he sou rce
o f t he su l pha te . The s i t ua t i on i s comp l i ca ted by t he f ac t t ha t ,
con t ra r y t o some ea r l y c onc lus i ons , t he amoun ts n eeded t o
op t im i se d i f f e ren t p rope r t i es , such as s t r eng th a t va r i ous ages
and d r y i ng sh r i nkage a re no t necessa r i l y t he same ; a l so , t he
amoun t needed t o op t im i se a g i ven p rope r t y i n a conc re te may
no t be t he same as t ha t requ i r ed i n a pas te o r mo r ta r (Tang
and Ga r tne r , 1988 ) .
Du r i ng t he ea r l y and m idd le pe r i ods o f r eac t i on i n a cemen t
pas te , gypsum d i sso l ve and reac t a t o r c l ose to t he su r f aces o f
t he c l i nke r g ra i ns , mo re spec i f i ca l l y t he a l um ina te and f e r r i t e
phases . The f ac to r mos t d i r ec t l y i n f l uenc ing t he cou rse o f t he
ea r l y r eac t i ons i s no t so much t he re l a t i ve amoun ts o f ca l c i um
su lpha te , a l um ina te and f e r r i t e phases , as t he r a te a t wh i ch t he
re l evan t i on i c spec ies a re made ava i l ab l e a t t he su r f ace o f t he
cemen t g ra i ns . O the r ma jo r f ac to r s a f f ec t i ng t he supp l y o f
t hese i ons a re the pa r t i c l e s i ze d i s t r i bu t i on o f t he ca l c i um
su lpha te and t he d i s t r i bu t i on i n space o f t he pa r t i c l es (Tay lo r ,
1995 ) . F r i g i one (1995 ) has , by mea s u r i ng the Ca 2 +
concen t ra t i on o f t he l i qu i d phase shown t ha t t he p resence o f
gypsum i nc reased t he C 3 S hyd ra t i on r a te , F i gu re 2 .2 .
The ca l c i um s i l i ca te hyd ra te r eac t i ons a re t he mos t i mpo r t an t
as t hese a re r espons ib l e f o r t he ma jo r i t y o f s t r eng th o f t he
ha rdened cemen t pas te ( hcp ) . The hyd ra t i o n p roduc t s o f t he
two ca l c i um s i l i ca tes a re s im i l a r and d i f f e r on l y i n t he t e rms o f
t he r a te a t wh i ch t hey oc cu r and i n t he amoun t o f ca l c i um
hyd rox i de f o rmed as seen i n equa t i on 2 .3 and 2 .4 . The reac t i on
o f t he C 3 S w i t h wa te r i s t he mo re rap id o f t he two .
2C 3 S + 6H → C 3 S 2 H 3 + 3CH ( equa t i on 2 .3 )
Al i te
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
2-7
F i gu re 2 .2 Changes i n Ca 2 + i n so l u t i on cu r i ng C 3 S hyd ra t i on vs .
t ime i n t he absence and p resence o f gypsum (F r i g i one , 1995 )
The C 2 S reac t i on i s s im i l a r , bu t i t t a kes p l ace a t a s l owe r r a te ,
con t r i bu tes l ess hea t t han t he C 3 S and i s r espons ib l e f o r t he
l a t e r s t r eng th deve lopmen t .
2C 2 S + 4H → C 3 S 2 H 3 + CH ( equa t i on 2 .4 )
Bel i t e
When wa te r i s added t o t he r eac t i ons above , t he ca l c i um
hyd rox i de i ons a re r ap id l y r e l eased i n t o t he so l u t i on and t he
pH o f t he so l u t i on r i ses r ap id l y t o ove r 12 . Du r i ng t h i s s t age a
cons ide rab le amoun t o f hea t i s evo l ved .
Wh i l e t he concen t ra t i on o f ca l c i um and hyd rox i de i ons a re
bu i l d i ng up , a do rman t pe r i od occu rs wh i ch co i nc i des w i t h t he
e t t r i ng i t e de lay f r o m the C 3 A reac t i on and he lps t o exp la i n why
pas te can rema in wo rkab le f o r so l ong . Once t he c r i t i ca l
concen t ra t i on o f t he i ons i s r eached t he CSH and CH s ta r t t o
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
2-8
c r ys ta l l i se ou t f r om the so l u t i on , s t r eng th i s deve loped and
wo rkab i l i t y i s l o s t .
2 .4 .2 Hyd ra t io n o f C 3 A
The reac t i on o f C 3 A w i t h wa te r i s ve r y f as t and i nvo l ves
r eac t i ons w i t h su l pha te i ons supp l i ed by t he d i sso lu t i on o f
gypsum ( see Equa t i ons 2 .5 and 2 .6 ) .
C 3 A + 3CSH 2 + 26H → C 3 A .3CS H 3 2 ( equa t i on 2 .5 )
Whe re :
H - Wa te r
CSH - Ca l c i um su lpha te (Gypsu m)
C 3 A .3CS H 3 2 - Ca l c i um Su lpha te A lum ina te Hyd ra te (E t t r i ng i t e )
The f o rma t i on o f e t t r i ng i t e s l ows down t he hyd ra t i on o f C 3 A by
c rea t i ng a ba r r i e r a round t he cemen t g ra i ns . A f t e r a ce r t a i n
po r t i on o f t he su l pha te has been consumed , t he e t t r i ng i t e
becomes uns tab le and a second reac t i on beg ins t o t ake p l ace
(Wa inwr i gh t , 2004 ) .
E t t r ing i t e
C 3 A + CSH + 10 H → C 3 A .CS H 1 2 ( equa t i on 2 .6 )
Mo nosu l pha te
I t i s no t un t i l t h i s second reac t i on occu rs t ha t t he pas te beg ins
t o s t i f f en s i gn i f i can t l y and wo rkab i l i t y beg ins t o d rop . The
ove ra l l C 3 A reac t i on p roduces a s i gn i f i can t quan t i t y o f hea t bu t
con t r i bu te l i t t l e t o t he s t r eng th .
An i nadequa te supp l y o f so l ub le ca l c i um su lpha te can resu l t i n
a r ap i d l oss o f wo rkab i l i t y known as f l a sh se t . Th i s i s
accompan ied by t he r e l ease o f hea t and i s i r r eve rs i b l e .
Howeve r , i f t oo h i gh a l eve l o f gyps um i s p resen t ; c r ys ta l s o f
gypsum c r ys ta l l i ze f r om the so l u t i on and cause a p l as te r o r
f a l se se t ( cemen t ) . I f m i x i ng con t i nues o r i s r esumed , t he i n i t i a l
l e ve l o r wo rkab i l i t y i s r es to red . The cemen t manu fac tu re r t hus
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
2-9
needs t o op t im i ze t he l eve l o f gypsum i n t he cemen t and ma tch
t h i s t o t he reac t i v i t y o f C 3 A p resen t . Th i s conc ep t i s i l l u s t r a t ed
i n F i gu re 2 .3 .
F i gu re 2 .3 Op t im i za t i on o f so l ub le ca l c i um su lpha te ( c emen ts )
(Newman , 2003 )
2 .4 .3 Hyd ra t io n o f C 4 A F
The f e r r i t e phase (C 4 AF) i s o f no g rea t impo r t ance compa red t o
t he o the rs . I t i s a s l ow reac t i on ( see equa t i on 2 .7 ) w i t h l i t t l e
hea t evo l ved and con t r i bu tes l i t t l e t o t he s t r eng th .
C 4 AF + 10H + 2CH → C 6 AFH 1 2 ( equa t i on 2 .7 )
Sulphofe r r i t e
2 .5 HEAT OF HYDR AT ION
The chem ica l r eac t i ons be tween unhyd ra ted cemen t and wa te r
du r i ng se t t i ng and ha rden ing re l ease hea t wh i ch r esu l t s i n a
r i se i n t empe ra tu re o f t he f r esh conc re te . I f op t imum
pe r f o rma nce i s t o be ach ieved f r o m the cemen t , i t i s t hough t
t ha t t he peak hyd ra t i on r a te assoc ia ted w i t h C 3 A shou ld be
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
2-10
de layed by SO 3 add i t i ons un t i l t he s i l i ca te hyd ra t i on r a te has
passed i t s peak .
2 . 5 .1 Opt im iza t ion o f Cement Su lpha te
Nev i l l e , ( 1995 ) sugges ted tha t t he op t imum g ypsum co n ten t be
de te rm ined by o bse rva t i on o f t h e gene ra t i on o f hea t o f
hyd ra t i on . Op t imum su lpha te w i t h r espec t t o s t r eng th
deve lopmen t and d imens iona l s t ab i l i t y occu r red when t he
dep le t i on o f so l ub le su l pha te used up by t he a l um ina te
hyd ra t i on occu r red a t a t ime l a t e r t han t he ma x imum hea t
evo lu t i on f r om th e ma in s i l i ca te hyd ra t i on peak (Sandbe rg ,
2004 ) . F i gu re 2 .4 shows an examp le o f hyd ra t i ng PC w i t h
s l i gh t l y h i ghe r t han op t imum su lpha te con ten t mon i t o red a t
r oom tempe ra tu re by an i so the rma l conduc t i on ca l o r ime te r .
The i n i t i a l peak i n F i gu re 2 .4 occu rs as soon as wa te r i s added
t o t he PC , r esu l t i ng f r om the e t t r i ng i t e be ing fo rmed i n t he C 3 A
reac t i on . The ca l c i um hyd rox ide i ons pass ing i n t o so l u t i on i n
t he cemen t m i xed w i t h wa te r i n i t i a l l y d i sp l ay s t r ong exo the rm ic
behav iou r by r ap id d i sso lu t i on and i n i t i a l hyd ra t i on o f ma in l y
t he a l um ina te phase as seen a t A i n F i gu re 2 .4 . I f s u f f i c i en t
su l f a t e i s ava i l ab l e i n t he so l u t i on , t he hyd ra t i on r a te r ap id l y
dec reases as t he a l um ina te r eac t s w i t h ca l c i um and su l f a t e t o
f o rm e t t r i ng i t e (B on t he cu r ve ) . The f o rma t i on o f e t t r i ng i t e
p reven t s f l a sh se t and a l l ows t he c onc re te t o be t r a nspo r t ed
and p l aced wh i l e i t i s s t i l l f l u i d . A f t e r some t ime t he s t r eng th
g i v i ng A l i t e hyd ra t i on t akes o f f , wh i ch r esu l t s i n a b road
exo the rm C . Se t usua l l y occu rs a t t he i n i t i a l pa r t o f t he A l i t e
exo the rm . The A l i t e and a l um ina te hyd ra t i on con t i nue i n
pa ra l l e l un t i l t he m i x tu re r uns ou t o f so l ub le su l pha te ( a t D ) ,
wh i ch i n i t i a t es t he f o rma t i on o f a l um ina tes w i t h l ess su l f a t e
t han e t t r i ng i t e (Sandbe rg , 2004 ) .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
2-11
F igu re 2 .4 Exa mp le o f no rma l hyd ra t i on o f Po r t l and cemen t
(Sandbe rg , 2004 )
A f t e r t he wa te r ha s been added t o t he cemen t t he f i r s t peak i n
t he r a te o f hea t evo lu t i on i s f o l l owed by a second peak some 4
t o 10 hou rs l a t e r . W i t h t he co r rec t amoun t o f gypsum the re
shou ld be l i t t l e C 3 A ava i l ab l e f o r r eac t i on a f te r a l l t he gypsum
has comb ined and no f u r t he r peak i n t he hea t l i be ra t i on shou ld
occu r . Thus op t imum gypsu m con ten t l eads to a des i rab le r a te
o f ea r l y r eac t i on and p reven t s l oca l h i gh concen t ra t i on o f
p roduc t s o f hyd ra t i on (Nev i l l e , 1995 ) . I n consequence t he s i ze
o f po res i n hyd ra ted cemen t pas te i s r educed and s t r eng th i s
i n c reased . The amoun t o f g ypsum re qu i r ed i nc reases w i t h t he
C 3 A con ten t and a l so w i t h t he a l ka l i con ten t o f t he cemen t .
I nc reas ing t he f i neness o f cemen t has t he e f f ec t o f i nc reas ing
t he quan t i t y o f C 3 A ava i l ab l e a t ea r l y s t ages , and t h i s r a i ses
t he gypsum requ i r emen t .
The amoun t o f gypsum added t o cemen t c l i nke r i s exp ressed as
t he mass o f SO 3 p resen t ; t h i s i s l im i t ed by t he SANS 50197 -
1 /SABS EN 197 -1 :2000 t o a ma x imu m o f 3 .5 %. The re i s usua l l y
f ound t o be an op t imum SO 3 con ten t ( 2 -3% fo r b i nde rs ) , beyond
wh i ch (> 4%) , compress i ve s t r eng th beg ins t o dec l i ne ( Lea ,
1998 ) . F r i g i one con f i rmed t h i s s t a temen t us i ng ISO-R ILEM
mor ta r p r i sms , f o r cemen ts w i t h a w ide range o f pa r t i c l e s i ze
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
2-12
d i s t r i bu t i ons , gypsum was added t o p reg round c l i nke r , and
f ound t ha t t he max i mum i n s t r eng th was no t sens i t i ve t o
pa r t i c l e s i ze g rad ing (F r i g i one and Mara , 1976 ) . Le r ch ’ s ,
( 1946 ) t es t r esu l t s i nd i ca te t ha t 2 . 5% added SO 3 may be
su f f i c i en t t o b r i ng t he r esu l t i ng PC to op t imum SO 3 l eve l .
2 .6 SPECIF I C SURF ACE AREA
At mos t manu fac tu r i ng p l an t s a ba l l m i l l i s used t o g r i nd t he
cemen t c l i n ke r . The p r i nc i pa l t es t ca r r i ed ou t a t a cemen t m i l l
i s t he f i neness tes t i n wh i ch t he spec i f i c su r f ace a rea i s
de te rm ined . The spec i f i c g rav i t y and f i neness o f ceme n t
i nc rease w i t h an i nc rease i n t he g r i nd i ng t ime . Bouzoubaâ e t a l
( 1997 ) f ound t ha t t h i s i nc rease i n f i neness was l ess s i gn i f i can t
beyond 2 hou rs . An op t imum o f 4 hou rs g r i nd i ng t ime was
es tab l i shed by Bo uzoubaâ , beyond wh i ch t he wa te r r e qu i r emen t
i nc reased and t he s t r eng th e i t he r dec reased o r d i d no t i n c rease
s i gn i f i can t l y .
The f i neness o f cemen t i s a ma jo r f ac to r i n f l uenc ing i t s r a t e o f
hyd ra t i on , s i nce the hyd ra t i on r eac t i on occu rs a t t he i n t e r f ace
w i t h wa te r ( Lea , 1988 ) . G re a te r cemen t f i neness i nc reases t he
ra te a t wh i ch cemen t hyd ra tes and t hus acce le ra tes s t r eng th
deve lopmen t . The e f f ec t s o f g rea te r f i neness on pas te s t r eng th
a re man i f es ted p r i nc i pa l l y du r i ng t he f i r s t seven days .
Po r t l and cemen t i s usua l l y g round t o a su r face a rea i n t he
r ange 300 – 350 m 2 / kg and rap id ha rden ing Po r t l and cemen t t o
400 – 550 m 2 / kg .
2 .7 PARTICL E S IZE D ISTRIBUT ION
The pa r t i c l e s i ze d i s t r i bu t i on cu r ve o f a ma te r i a l desc r i bes two
p rope r t i es o f t he ma te r i a l name l y mean pa r t i c l e s i ze as we l l as
t he d i s t r i bu t i on o f o t he r s i zes abou t t he mean . The cu rve i s
usua l l y d rawn as t he cumu la t i ve pe rcen tage -va lues on t he y -
ax i s o f pa r t i c l es sma l l e r t han t he co r respond ing s i zes on t he x -
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
2-13
ax i s . The x -ax i s i s d rawn to a l og sca le t o accommod a te l a rge
ranges o f pa r t i c l e s i zes . The shape o f t he cu r ve g i ves an
i nd i ca t i on o f t he con t i nu i t y i n s i ze d i s t r i bu t i on and t he s l ope
desc r i bes t he w ideness o r range o f t he s i ze d i s t r i bu t i on .
Pa r t i c l e s i ze d i s t r i bu t i ons o f i n t e rg round b l ended cemen ts a re
d i f f e ren t t han t ha t o f sepa ra te l y g round cemen ts (E rdogdu ,
1999 ) . The pa r t i c l e s i ze d i s t r i bu t i on p roduced when a ma te r i a l
i s g round becomes w ide r as t he ma te r i a l becomes eas ie r t o
g r i nd . Du r i ng t he i n t e rg r i nd i ng o f cemen t cons t i t uen t s o f
d i f f e r i ng g r i ndab i l i t y , t he pa r t i c l e s i ze d i s t r i bu t i on o f t he
ma te r i a l wh i ch i s ha rde r t o g r i nd becomes na r rowe r , t he eas ie r
t he o the r componen t i s t o g r i nd . Conve rse l y , t he pa r t i c l e s i ze
d i s t r i bu t i on o f t he ma te r i a l wh i ch i s eas i e r t o g r i nd becomes
w ide r t he ha rde r t he o the r componen t i s t o g r i nd ( Lea , 1988 ) .
App rox ima te l y 95% o f cemen t pa r t i c l es a re sma l l e r t han 45µm,
w i t h t he ave rage pa r t i c l e a round 15µm. Bye , ( 1999 ) suppo r t ed
t he gene ra l l y he ld v i ew t ha t t he 3 -30µm f r ac t i on makes a ma jo r
con t r i bu t i on t o t he 28 -day s t r eng th . The range <3µm i s
impo r tan t f o r ach iev i ng h i gh 1 -day s t r eng ths .
2 .7 .1 Ros in -Ra mmler d is t r ibu t ion func t ion
I n sea rch ing f o r a pa rame te r , wh i ch w i l l p rov i de a mo re
r ep resen ta t i ve desc r i p t i on o f t he pa r t i c l e s i ze d i s t r i bu t i on , t h e
Ros in -Rammle r f u nc t i on was i nves t i ga ted .
F rom a p robab i l i t y po in t o f v i ew Ros in and Rammle r
i nves t i ga ted t he pa r t i c l e s i ze d i s t r i bu t i on o f c rushed coa l and
deve loped a f unc t i on t ha t desc r i bes t he d i s t r i bu t i on as (Ros in ,
1933 ) :
ƒ ( x ) = exp ( -bx n ) ( equa t i on 2 .8 )
Whe re :
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
2-14
b - F i neness cha rac te r i s t i c measu re o f t h e ma te r i a l be i ng
ana l ysed .
n - A mea s u re o f t he r ange o f pa r t i c l e s i zes .
Ros in and Rammle r a l so found t ha t t he f unc t i on does no t on l y
app l y t o c rushed coa l bu t a l so t o va r i ous o the r powered
ma te r i a l s .
The f unc t i on was mod i f i ed as f o l l ows :
RR = exp – (x /X o ) n ( equa t i on 2 .9 )
Whe re :
The we igh t i ng f unc t i on ƒ ( x ) i s deno ted as RR .
X o – t he abso lu te s i ze cons tan t o r pos i t i on pa rame te r ( i t
r ep resen ts t he pa r t i c l e s i ze f o r wh i ch 36 .8% o f t he pa r t i c l es
a re coa rse r ) .
Tak ing t he doub le l oga r i t hm o f equa t i on 2 .9 we ob ta i n :
l n l n (1 /RR) = n ( l nx - l nX o ) ( equa t i on 2 .10 )
Equa t i on 2 .10 desc r i bes a s t r a i gh t l i ne p l o t w i t h a coo rd i na te
sys tem made up o f a l og sca le absc i ssa f o r t he pa r t i c l e s i ze x ,
and an o rd i na te w i t h a doub le l oga r i t hm o f t he r ec i p roca l o f t he
r es i due RR. The s l ope o f t he s t r a i gh t l i ne i s n and t he l i ne
i n t e r cep t t he ho r i zon ta l ax i s a t a va l ue desc r i b i ng t he pa r t i c l e
s i ze x (O lo runsogo , 1990 ) . A h y po the t i ca l examp l e o f t he
d i ag rammat i c r ep resen ta t i on o f t he pa r t i c l e s i ze d i s t r i bu t i on by
t he Ros in -Rammle r d i s t r i bu t i on f unc t i on i s shown i n F i gu re 2 .5 .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
2-15
F igu re 2 .5 D iag rammat i c r ep resen ta t i on o f Ros in -Ramle r
d i s t r i bu t i on f unc t i on (Wa inwr i gh t and O lo runsogo , 1999 )
F i gu re 2 .5 ( a ) shows t he t yp i ca l pa r t i c l e s i ze d i s t r i bu t i on o f
f ou r d i f f e ren t samp les hav ing t he same n and d i f f e ren t Xo .
Th i s i l l u s t r a t i on shows t ha t t he samp le r ep resen ted by t he f ou r
p l o t s m igh t have s im i l a r r anges o f s i ze d i s t r i bu t i on ( deno ted by
equa l n ) bu t w i t h poss ib l e va r y i ng deg rees o f f i neness
( i nd i ca ted by t he va r i ous X o ) . The samp le r ep resen ted by p l o t 1
be ing t he f i nes t and t he one by p l o t 4 t he coa rses t o f t he f ou r .
S im i l a r l y , F i gu re 2 .5 ( b ) i l l us t r a tes a s i t ua t i on whe reby t he f ou r
samp les m igh t be o f t he same f i neness (bec ause o f t he same
X o ) bu t poss ib l y w i t h d i f f e ren t s i ze r anges (Wa inwr i gh t and
O lo runsogo , 1999 ) .
2 .8 CONCLUSION
• Tes t r esu l t s i nd i ca te t ha t 2 . 5% added SO 3 may be
su f f i c i en t t o b r i ng t he r esu l t i ng PC to op t imum SO 3 l eve l .
• The spec i f i c g rav i t y and f i neness o f cemen t i nc rease w i t h
an i nc rease i n t he g r i nd i ng t ime .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
2-16
• An op t imum o f 4 hou rs g r i nd i ng t ime was es tab l i shed
beyond wh i ch t he wa te r r equ i r emen t i nc rease and t he
s t r eng th e i t he r dec rease o r d i d no t i n c rease s i gn i f i can t l y .
• G rea te r cemen t f i neness i nc reases t he ra t e a t wh i ch
cemen t hyd ra tes and t hus acce le ra tes s t r eng th
deve lopmen t .
• The pa r t i c l e s i ze d i s t r i bu t i on p roduced when a ma te r i a l i s
g round becomes w ide r as t he ma te r i a l becomes eas ie r t o
g r i nd .
• App rox ima te l y 95% o f cemen t pa r t i c l es a re sma l l e r t han
45µm, w i t h t he ave rage pa r t i c l e a round 15µm.
• The 3 -30µm f r ac t i on make s a ma jo r con t r i bu t i on t o t he
28 -day s t r eng th . The range <3µm i s impo r tan t f o r
ach iev i ng h i gh 1 -day s t r eng ths .
• The Ros in -Ramml e r d i s t r i bu t i on f unc t i on can be eva lu a ted
as a me thod p rov i d i ng an easy me ans o f desc r i b i ng t he
pa r t i c l e s i ze d i s t r i bu t i on quan t i t a t i ve l y .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3-1
3. COMPOSITION AND PROPERTIES OF COAL ASH 3 .1 INTRODUCTION
Sus ta inab le deve lopment can be de f ined , as deve lopment , wh ich
meets the needs o f peop le l i v ing today w i thou t compromis ing the
ab i l i t y o f fu tu re genera t ions to mee t the i r own needs . I t requ i res
a long- te rm v i s i on o f i ndus t r ia l p rog ress , p rese rv ing the
founda t ions upon wh ich human qua l i t y o f l i f e depends : respec t
fo r bas ic human need and loca l and g loba l ecosys tems.
Us ing by -p roduc ts f rom o ther i ndus t r ies as raw ma te r ia l i s a
huge oppor tun i t y fo r the cemen t i ndus t r y to reduce i t s
env i ronmenta l impac t , because i t a l l ows compan ies to access
ma te r i a l s fo r use i n the k i l n and the m i l l w i thou t ex t rac t ing them
d i rec t l y f rom the g round . There a re a number o f m inera l by -
p roduc ts tha t con ta in use fu l ma te r ia l s tha t can be ex t rac ted f o r
use in cement p roduc t ion , o r i n mak ing concre te . Typ ica l
add i t i ves inc lude s lag , coa l ash l i ke f l y ash and bo t tom ash , by -
p roduc ts f rom b las t fu rnaces and power gene ra t ion .
Cement , a f i ne g rey powder , se ts a f te r a few hours when mixed
w i th wa te r , and then hardens in a f ew days i n to a so l i d , s t rong
ma te r i a l . V i r t ua l l y a l l t he cement p roduced g loba l l y i s m ixed w i th
sand , aggrega tes and wa te r and used to make conc re te and
mor ta rs .
Cement ex tende rs a re used as a subs t i tu te f o r some o f t he PC in
concre te . The ma in reason fo r the use o f ex tenders i s t he va r ie t y
o f use fu l enhancements , wh ich they g i ve to the concre te
p roper t i es . F l y ash i s one o f the cement ex tende rs common l y
used in Sou th A f r i ca . F l y ash cons is ts o f f i ne l y d i v i ded ashes
p roduced by bu rn ing pu lve r i sed coa l i n power s ta t i ons .
Gas i f i ca t i on ash i s a p roduced as a by -p roduc t du r ing the
gas i f i ca t i on o f coarse coa l . The p roper t i es o f f l y ash can be
used as a gu ide l ine to i nves t iga te o the r ashes fo r use as cemen t
ex tenders in conc re te .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3-2
In t h i s chap te r , the use o f coa l combus t ion by-p roduc ts ,
spec i f i ca l l y f l y ash , i n conc re te w i l l be d i scussed . Cons ide ra t ion
w i l l be g i ven to p roper t i es l i ke shape , pa r t i c le s i ze ,
m inera log ica l and chemica l compos i t i on , du rab i l i t y and the
chemica l requ i rements f o r us ing f l y ash as a cement ex tender .
Th is w i l l p rov ide adequa te unde rs tand ing o f the advan tages tha t
by -p roduc ts have to bo th the cement i ndus t ry and the
env i ronment .
3 .2 COAL ASH
Cur ren t l y , c lose to a b i l l i on tons o f coa l i s bu rned annua l l y i n
the wor ld to gene ra te e lec t r i c i t y and as a resu l t , near l y 130
m i l l i on tons o f coa l combus t ion by -p roduc ts (CCBs) a re
p roduced . One- th i rd o f t hese CCBs a re u t i l i zed , wh i l e the res t
a re d i sposed o f ma in l y i n l and f i l l s (Schwar tz , 2003) . Inc reas ing
cos ts and he igh tened regu la t ions a re mak ing the d i sposa l o f
CCBs an undes i rab le op t ion . U t i l i za t ion o f CCBs as raw
ma te r i a l s resu l t s i n numerous bene f i t s , i nc lud ing :
• A dec rease in t he demand fo r l and f i l l space
• Conserva t ion o f na tu ra l resources
• A c leaner sa fe r env i ronment
• Reduced ca rbon d iox ide emiss ions
• S ign i f i can t economic sav ings fo r end use rs
• A boos t i n economic deve lopment
• Reduced overa l l cos t o f genera t i ng e lec t r i c i t y
E lec t r i c i t y i s the fue l o f the “ In fo rmat ion age ” and power p lan ts
tha t bu rn coa l accoun t fo r more than ha l f o f the e lec t r i c i t y
p roduced . These power p lan ts a l so p roduce coa l combus t ion by -
p roduc ts l i ke f l y ash (wh ich i s cap tu re f rom the exhaus t o f t he
bo i le r ) and bo t tom ash (wh ich i s heav ie r and fa l l s to the bo t tom
o f the bo i le r ) . CCBs a re cons ide red to be fou r d i s t i nc t and
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3-3
ex t reme ly d i f f e ren t mate r ia l s , as seen in F igu re 3 .1 (Amer ican
Coa l Ash Assoc ia t i on , 1997 ) .
Coa l bo t tom ash and bo i le r s lag a re the coarse , g ranu la r ,
i ncombus t ib le by -p roduc ts t ha t a re co l lec ted f rom the bo t tom o f
fu rnaces tha t bu rn coa l fo r the genera t i on o f s team and the
p roduc t ion o f e lec t r i c i t y . Bo t tom ash i s a da rk g ray , g ranu la r ,
po rous , p redominan t l y sand s i ze ( -12 .7mm) ma te r i a l (Babcock ,
1978 ) . Ma te r i a l d rops i n to a wa te r f i l l ed hopper a t the bo t tom o f
the fu rnace . The ma te r i a l i s removed by means o f h igh -p ressure
wa te r j e ts and conveyed by s lu i ceways e i the r to a d i sposa l pond
o r to a decan t bas in . F rom he re the mate r ia l i s dewate red ,
c rushed and s tockp i led fo r d i sposa l o r use (Hec t , 1975) .
Bo t tom ash app l i ca t ions a re snow and i ce con t ro l , as aggrega te
in l i gh twe igh t conc re te masonry un i t s , and raw feed mate r i a l f o r
the p roduc t ion o f PC. Bo t tom ash has a lso been used as a road
base and subbase agg rega te , s t ruc tu ra l f i l l ma te r ia l (ASTM
E1861-97 ) , and as f i ne aggrega te in aspha l t pav ing .
F l ue gas desu lphu r i sa t i on (FGD) gypsum i s a l so known as
sc rubbe r gypsum. FGD gypsum i s t he by -p roduc t o f an a i r
po l l u t i on con t ro l s ys tem th a t r emo ves su lphu r f r om th e f l ue gas
i n ca l c i um-based sc rubb ing sys tems . I t i s p roduced by
emp loy i n g f o r ced ox i da t i on i n t he sc rubbe r and i s composed
mos t l y o f ca l c i um su lpha te .
The ma jo r i t y o f FDG-p rod uced gypsum used i n t he Un i t ed
S ta tes (Amer i can Coa l Ash Assoc ia t i on , 1997 ) i s emp loyed f o r
wa l l boa rd , wh i ch reduced the need f o r m in i ng na tu ra l gypsum.
As an add i t i ve i n PC , FDG gypsum i s used t o r e ta rd se t t i ng .
Th i s enab les we t cemen t i n r eady -m ix t r uck s t o be t r anspo r t ed
g rea te r d i s t ances wh i l e rema in i ng wo rkab le . Gypsum ’s h i gh
pe rmeab i l i t y ( 10 -3cm/sec ) makes i t an exce l l en t so i l
cond i t i one r . S te f f an ( 1991 ) i nd i ca tes t ha t FGD g ypsum o f f e r s
seve ra l ma jo r be ne f i t s as a so i l amendme n t . These i nc l ude
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3-4
ad jus tmen t o f so i l pH and means o f keep ing peanu t s and o the r
c rops d i sease - f r ee .
F igu re 3 .1 Coa l combus t i on by -p rodu c t s
The f ou r t h CCB i s f l y ash wh i ch i s mos t o f t en used i n conc re te
as a r ep lacemen t f o r pa r t o f t he PC i n t he m ix des ign . The use
o f f l y ash as an ex tende r i n conc re te w i l l be d i scussed l a t e r i n
t h i s chap te r .
3 .3 POZZOLANIC REACTION
The Amer i can Soc ie t y f o r Tes t i ng Ma te r i a l s (ASTM) de f i nes a
pozzo lan as ‘ a s i l i ceous o r s i l i ceous and a l um inous ma te r i a l ,
wh i ch i n i t se l f possesses l i t t l e o r no cemen t i t i ous p rope r t y bu t
wh i ch w i l l , i n f i ne l y d i v i ded f o rm and i n t he p resence o f
mo i s tu re , chem ica l l y r eac t w i t h ca l c i um hyd rox i de a t o rd i na ry
t empe ra tu re t o f o rm compounds possess ing cemen t i ng
p rope r t i es ’ .
As a pozzo lan ic ma te r i a l f l y ash con ta ins ac t i ve s i l i ca (S iO 2 ) ,
and i s no t cemen t i t i ous in i t se l f bu t w i l l chemica l l y reac t w i th
ca lc ium hydrox ide in the p resence o f mo is tu re to fo rm
cement i t i ous compounds ( I l l s ton , 2001) . When a pozzo lan ic
ma te r i a l i s used in con junc t i on w i th a PC, the ca lc ium hyd rox ide
tha t takes pa r t i n the pozzo lan ic reac t ion i s t ha t p roduced f rom
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3-5
the cement hyd ra t ion . More quan t i t i es o f ca l c ium s i l i ca te
hydra te a re p roduced (see equa t ion 3 .1 ) .
2S + 3CH → C 3 S 2 H 3 (equa t ion 3 .1 )
I t i s c l ea r t ha t t he pozzo lan ic reac t ion i s secondary to t he
hydra t ion o f PC. The deg ree o f hyd ra t ion o f f l y ash i s i nc reased
in the p resence o f gypsum because the su r face i s ac t i va ted by
the des t ruc t i on o f the s t ruc tu re o f the g lass and c rys ta l l i ne
phases caused by the d i ssoc ia t ion o f A l 2 O 3 reac t i ng w i th SO 4-
(Uch ikawa, 1986) . The p roduc ts o f the pozzo lan ic reac t i on make
the i r own con t r ibu t ion to the s t reng th and o the r p roper t i es o f t he
cement and conc re te .
3 .4 FLY ASH
F l y ashes (FA ) cons i s t o f f i ne l y d i v i ded ashes p roduced by
bu rn i ng pu l ve r i sed coa l i n power s t a t i ons as seen i n F i gu re 3 .2 .
They a re r emoved f r om the combus t i on gases and co l l ec ted by
spec ia l mechan i ca l dev i ces and e l ec t r os ta t i c p rec i p i t a t o r s .
Ow ing t o t he h i gh t empe ra tu res r eached du r i ng t he
i ns tan taneous bu rn i ng o f coa l , mos t o f t he m ine ra l componen t
con ta i ned i n t he coa l me l t s and f o rms sma l l f used d rops . The
subsequen t sudden coo l i ng t r ans fo rms t hem pa r t l y o r en t i r e l y
i n t o sphe r i ca l g l ass pa r t i c l es . The recogn i t i on t ha t f l y ash
exh ib i t s pozzo lan i c p rope r t i es has l ed t o i t s use as a
cons t i t uen t o f conc re te . F l y ashes con ta i n me tas tab le
a l um inos i l i ca tes tha t w i l l r eac t w i t h ca l c i um i ons i n t he
p resence o f mo is tu re t o f o rm ca l c i um s i l i ca te hyd ra tes
(Massazza , 1998 ) . F l y ash p roduced i n Sou th A f r i ca i s a f i ne
powde r , t he pa r t i c l es o f wh i ch a re round ho l l ow sphe res ( see
F igu re 3 .3 ) .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3-6
F igu re 3 .2 A modern pu l ve r i sed coa l - f i red the rma l power s ta t ion
(K rüge r , 1999 ) .
F l y ash i s used i n conc re te e i the r as pa r t o f b lended cement o r
as a separa te componen t added a t the s tage when the concre te
m ix i s p repared . The inc lus ion o f f l y ash in conc re te a f fec ts a l l
aspec ts o f conc re te . As pa r t o f t he compos i te conc re te mass ,
f l y ash ac ts bo th as a f i ne aggrega te and as a cement i t i ous
componen t . I t i n f l uences the rheo log ica l p roper t i es o f the f res h
concre te and the s t reng th , f i n i sh , po ros i t y , and durab i l i t y o f the
ha rdened mass as we l l as the cos t and ene rgy consumed in
manu fac tu r ing the f i na l p roduc t (Massazza , 1998) .
3 .4 .1 Phys ica l Proper t ies
F ly ash par t i c les a re mos t l y spher i ca l i n shape (see F igu re 3 .3 )
w i th s i zes rang ing f rom approx ima te l y 1 to 100μm in d iamete r ,
w i th an ave rage s i ze o f 20μm (Care t te , 1986) . The su r face a rea
o f f l y ash pa r t i c l es va ry f rom 2000 cm 2 /g to 10 000 cm 2 /g
depend ing on the p ropor t i on o f f i ne pa r t i c l es in the f l y ash .
E rdogdu (1998 ) f ound tha t conc re te con ta in ing a f i ne r f rac t ion o f
f l y ash gave a be t te r compress ive s t reng th than tha t w i thou t f l y
ash o r conc re te con ta in ing coarse r f l y ash . The pa r t i c le s i ze
d i s t r i bu t i on , shape and su r face cha rac te r i s t i c s o f f l y ash have a
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3-7
cons ide rab le i n f l uence on the wa te r requ i rement and workab i l i t y
o f f resh l y made concre te and on the ra te o f s t reng th
deve lopment i n ha rdened concre te .
F igu re 3 .3 E lec t ron m ic roscope pho tograph o f f l y ash .
3 .4 .2 Chemica l Composi t ion
The chemica l compos i t i on o f f l y ash depends on the
charac te r i s t i cs and compos i t i on o f the coa l bu rned in power
s ta t ions . The chemica l ana lys is o f f l y ashes by means o f X - ray
f l uo rescence (XRF) and spec t rome t ry techn iques shows tha t
S iO 2 , A l 2 O 3 , Fe 2 O 3 , and CaO are the ma jo r cons t i tuen ts o f mos t
f l y ashes . Tab le 3 .1 shows the t yp ica l chemica l compos i t i on o f
f l y ash .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3-8
Tab le 3 .1 Typ ica l chemica l compos i t i on o f f l y ash (Add is , 2001)
Oxide % By mass S iO 2 45-50
Al 2 O 3 25-30
CaO 4-8
FeO 9 -11
MgO 2-4
Na 2 O + 0 .658K 2 O 1 -3
3 .4 .3 Minera log ica l Compos i t ion
Both the t ype and source o f f l y ash i n f l uence i t s m inera log ica l
compos i t i on . Due to the rap id coo l i ng o f bu rned coa l i n t he
power p lan t , f l y ash cons is ts o f nonc rys ta l l i ne pa r t i c l es (≤ 90%) ,
o r g lass and a sma l l amoun t o f c r ys ta l l i ne mate r ia l .
I n add i t i on to a subs tan t i a l amoun t o f g lassy ma te r i a l , each f l y
ash may con ta in one o r more o f the fou r ma jo r c rys ta l l i ne
phases : qua r tz , mu l l i t e , magne t i te , and hemat i te . I n
subb i tuminous f l y ashes , the c rys ta l l i ne phases may inc lude C 3 A,
C 3 A 3 S , ca lc ium su lpha te , and a lka l i su lpha tes (Metha , 1989) .
The reac t i v i t y o f f l y ashes i s re la ted to t he noncrys ta l l i ne phase
o r g lass . D iamond (1981) po in ted ou t tha t t he compos i t i on o f
g lass in l ow-ca lc i um f l y ashes i s d i f fe ren t f rom tha t i n h igh -
ca lc ium f l y ashes . X- ray d i f f rac t ion (XRD) ind ica tes tha t Sou th
A f r i can f l y ash cons is ts m inera log ica l l y ma in ly o f g lass and
some low-quar tz (S iO 2 ) , mu l l i t e (A l 6 S i 2 O 1 3 ) and some qu ick l ime
(CaO) .
3 .4 .4 Chemica l Spec i f ica t ions
I n Sou th A f r i ca f l y ash shou ld comp ly w i th t he requ i rements o f
the Sou th A f r i can s tanda rd spec i f i ca t ion fo r Po r t l and cement
ex tenders (SANS 1491-2 :2005 / SABS 1941-2 :2005) . F l y ash
comp ly ing w i th SANS 149-2 may be used as a cement ex tender
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3-9
w i th Por t l and cement fo r use in conc re te when i t con fo rms to
Tab le 3 .2 .
Loss on ign i t i on , the we igh t l oss o f f l y ashes burned a t
tempera tu res ≤ 1000°C, i s re la ted to the p resence o f ca rbona tes ,
comb ined wa te r i n res idua l c lay m inera ls , and combus t ion o f
f ree ca rbon . The wa te r requ i red fo r wo rkab i l i t y o f mor ta rs and
concre tes depends on the ca rbon con ten t o f f l y ashes : the
h ighe r the ca rbon con ten t o f a f l y ash , the more wa te r i s needed
to p roduce a pas te o f no rma l cons is tency .
Tab le 3 .2 Chemica l spec i f i ca t ions fo r cement ex tenders . (SANS
1491-2 :2005 / SABS 1941-2 :2005)
Test F ly ash max a l lowed
Su lphur t r i ox ide con ten t , % (m/m) 2 .5
Loss on i gn i t i on , % (m/m) 5 .0
F ree wa te r con ten t , % (m/m) 1 .0
F ineness , res idue re ta ined on a s ieve w i th square aper tu res o f nomina l s i ze 45μm, % (m/m) 12 .5
Wate r requ i rement , % o f con t ro l 95
S t reng th fac to r , % 6
Soundness , expans ion , mm 5
3 .5 INFLUENCE OF FLY ASH ON THE PROPERTIES OF CONCRETE
3 .5 .1 Fresh Concrete
Al though concre te i s i n the f resh s ta te fo r on l y a few hours , the
p roper t i es o f f resh conc re te a re impor tan t because they
in f l uence the hand l ing o f t he conc re te , t he degree to wh ich i t
can be compac ted and the un i fo rm i t y o f d i s t r i bu t ion o f
cons t i tuen ts w i th in the conc re te .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3-10
3 .5 .1 .1 Wate r Demand
Dav is (1937) no ted , f l y ash d i f fe rs f rom o ther pozzo lans , wh ich
inc rease the wa te r requ i rement o f conc re te m ixes . The improved
workab i l i t y a l l ows a re duc t i on in the amoun t o f wa te r used i n
conc re te . Par t i a l rep lacement o f OPC by f l y ash , i n conc re te
reduces the wa te r requ i rement to ob ta in a g i ven cons is tency
(Ma lho t ra , 1996) . Th is i s genera l l y a t t r i bu ted to t he spher i ca l
shape and smooth tex tu re o f the f l y ash pa r t i c l es .
Accord ing to Owens (1979) t he ma jo r fac to r i n f l uenc ing the
e f fec ts o f ash on the workab i l i t y o f conc re te i s the p ropor t i on o f
coarse mate r i a l (>45µm) i n the ash . Very f i ne pa r t i c l es o f f l y ash
ge t abso rbed on the oppos i te l y charged su r face o f cement
pa r t i c l es and p reven t them f rom f loccu la t ion . The cemen t
pa r t i c l es a re thus e f fec t i ve l y d i spersed and w i l l no t t rap la rge
amounts o f wa te r , wh ich means tha t the sys tem w i l l have a
reduced wa te r requ i rement fo r f l ow. I n add i t i on , Por t l and cemen t
pa r t i c l es a re mos t l y i n t he s i ze range o f 1 t o 50μm, wh ich cause
the m ic ro f i ne pa r t i c les o f f l y ash to reduce the vo id space and
co r respond ing l y the wa te r requ i rement .
The re la t ionsh ip be tween the amoun t o f wa te r and the
pe rcen tage o f f l y ash rep lacement fo r the same workab i l i t y w i th
21 , 28 and 34 MPa nomina l -s t reng th conc re te can be seen i n
F igu re 3 .4 . As the amount o f f l y ash inc reased in the m ix tu re ,
the wa te r requ i rement dec reased (Na i k , 1990) .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3-11
F igu re 3 .4 Re la t ionsh ip be tween wa te r requ i rement and cemen t
rep lacement w i th f l y ash (Na ik , 1990 )
3 .5 .1 .2 Workab i l i t y
The ACI Commi t tee 116R-00 :2000 has p rov ided the mos t
su i tab le de f in i t i on o f workab i l i t y , wh ich reads as fo l l ows :
“ tha t p roper t y o f f resh l y m ixed concre te o r mor ta r wh ich
de te rm ines the ease and homogene i t y w i th wh ich i t can be
m ixed , p laced , conso l ida ted and f i n i shed . ”
The workab i l i t y ( f l u id i t y ) o f a Po r t l and concre te can be improved
when par t o f the OPC i s rep laced w i th f l y ash . B rown (1982 )
found tha t bo th s lump and V-B workab i l i t y improved w i th
inc reased ash subs t i tu t i ons . The ex ten t o f t he improvements
depends on the f i neness and ca rbon con ten t o f the f l y ash .
Rheo log i ca l p rope r t i es and f l u id i t y has been found to depend on
the pa r t i c le s i ze d i s t r i bu t ion o f cemen t (Gosh , 1983 ) . Lee (2002 )
found tha t the f l u i d i t y o f a f l y ash -cement sys tem inc rease as
the pa r t i c le s i ze d i s t r i bu t ion becomes w ide r . When workab i l i t y i s
kep t cons tan t t he wa te r con ten t o f a f l y ash m ix dec reases w i th
an inc rease in t he f i neness o f the f l y ash .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3-12
3 .5 .2 Hardened Concre te
The s t reng th o f ha rdened concre te i s o f fundamenta l impor tance
to s t ruc tu ra l des igners . I t i s a l so ex tens i ve l y used as an i ndex
o f o the r p rope r t i es and o f conc re te qua l i t y .
3 .5 .2 .1 Compress i ve S t reng th Deve lopment
The measured compress i ve s t reng th o f conc re te depends on the
in t r i ns i c p roper t i es o f the concre te . Many va r i ab les i n f l uence the
s t reng th deve lopment o f f l y ash conc re te , these be ing :
• p roper t i es o f f l y ash
• chemica l compos i t i on
• pa r t i c l e s i ze
• reac t i v i t y
• t empera tu re and cu r ing cond i t i ons
A t ea r l y ages the compress ive s t reng ths (up to 28 days ) o f a l l
conc re tes con ta in ing f l y ash a re lower than tha t o f t he
co r respond ing concre te con ta in ing norma l Po r t l and cemen t .
A f te r 28 days , i f we t cu r ing i s con t inued , the compress i ve
s t reng th o f f l y ash concre te w i l l be h igher t han the Por t l and
concre te (K rüge r , 1999 ) . Th is i s demons t ra ted in F igu re 3 .5 .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3-13
F igu re 3 .5 Deve lopment o f compress ive s t reng ths o f Por t l and
cement and f l y ash concre tes ( f rom Krüge r , 1999)
Par t i c le s i ze can in f l uence the s t reng th deve lopmen t i n two
ways . Pa r t i c les la rger t han 45μm in f luence wa te r requ i remen ts
adverse l y . They coun te rac t t o the needs o f the me thods used to
compensa te fo r the s low ra te o f reac t ion o f f l y ash a t ea r l y ages .
Cement ing ac t i v i t y occurs on the su r face o f the so l i d phases ,
th rough p rocesses invo l v i ng the d i f fus ion o f ma te r ia l s i n
concen t ra ted pas tes . F igu re 3 .6 shows tha t f i ne r f l y ashes
impar ted g rea te r compress i ve s t reng ths (Josh i , 1982) .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3-14
F igu re 3 .6 E f fec t o f coarse f rac t ions o f f l y ash on compress i ve
s t reng th deve lopment o f conc re tes (Josh i , 1982)
Conc re te con ta in ing f l y ash shows s t reng th ga in as a
consequence o f hea t ing in con t ras t to the loss o f s t reng th tha t
occurs w i th no rma l Por t l and cement (Ma lho t ra , 1996) . Th is
p roper t y o f f l y ash i s o f g rea t va lue i n the cons t ruc t i on o f mass
concre te o r i n conc re te cons t ruc t i on a t e leva ted tempera tu res .
The e f fec t o f cu r i ng tempera tu re on the s t reng th deve lopment o f
conc re te con ta in ing f l y ash can be seen in F igu re 3 .7 .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3-15
F igu re 3 .7 Compress i ve s t reng ths o f PC and PC/30FA a t
d i f f e ren t t empera tu res (K rüger , 1999 ) .
3 .5 .2 .2 F lexura l S t rength
There i s a genera l t rend fo r the f l exu ra l to compress i ve s t reng th
ra t io t o i nc rease w i th an i nc rease in f l y ash con ten t . The resu l t s
p resen ted in F igu re 3 .8 , po in ts ou t tha t t he inc rease i s s l i gh t fo r
wa te r cement (w /c ) ra t i os a round 0 .5 . The f l exu ra l t o
compress ive s t reng th ra t io o f Por t l and cement conc re te i s
s im i l a r t o tha t o f PC/FA conc re te o f s im i l a r s t reng th . Compar ing
the f l exu ra l to compress i ve s t reng th ra t ios o f t he PC and PC/FA
mor ta r a t s im i la r compress i ve s t reng th , a l though no t reached a t
the same age , the resu l t s i nd ica te tha t the ra t io f o r t he PC/FA
mor ta r i s somewhat h ighe r t han tha t f o r the PC mor ta r .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3-16
F igure 3 .8 The in f l uence o f FA con ten t o f the cement i t i ous
ma te r i a l on the f l exu ra l / compress i ve s t reng th ra t i o o f conc re te
(K rüge r , 1999 )
3 .5 .2 .3 Modulus o f E las t ic i ty
The modu lus o f e las t i c i t y o f a mate r ia l i s de f i ned by the s t ress :
s t ra in cu rve . The h igher the e las t i c modu lus , the more res is tan t
the ma te r ia l i s t o de fo rmat ion .
There appears to be no s ign i f i can t d i f f e rence be tween the
modu lus o f e las t i c i t y o f conc re te w i th o r w i thou t f l y ash a t 28
days . However , l i ke compress ive s t reng th , conc re te w i th f l y ash
has a lower modu lus a t ea r l y age s t reng th and h ighe r modu lus
a t u l t ima te s t reng th compared w i th concre te w i thou t f l y as h
(Lane , 1982) . The e f fec t o f f l y ash con ten t on the re la t i onsh ip
be tween compress ive s t reng th and e las t i c i t y can be seen in
F igu re 3 .9 .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3-17
F igu re 3 .9 The in f l uence o f FA on the e las t i c modu lus /
compress ive s t reng th o f conc re te (K rüge r , 1999)
3 .5 .2 .4 Dry ing Shr inkage
When a hydrau l i c cemen t -bonded p roduc t such as conc re te
looses i t s f ree mo is tu re , i t sh r inks (d ry ing sh r inkage) and when
i t ga ins i n mo is tu re con ten t , i t expands (we t t i ng expans ion ) . The
d imens iona l change w i th va r ia t i on in mo is tu re con ten t o f
conc re te i s and impor tan t p rope r t y , because i f d i f f e ren t ia l
d imens iona l movement i n t he conc re te due to such a change i s
excess i ve , c rack ing may occur . I f a d imens iona l l y s tab le
aggrega te i s used , d ry ing sh r inkage and we t t i ng expans ion can
a lmos t exc lus ive l y be a t t r i bu ted to the b inder and i s a f fec ted by
fac to rs such as b inder con ten t , wa te r / cement ra t io , cu r ing and
the s t reng th o f the conc re te (Add is , 2001) .
Work by Gr ieve (1991) on concre te made w i th a Sou th A f r i can
f l y ash , showed tha t fo r s im i la r exposure cond i t i ons , the d ry ing
sh r inkage o f such conc re tes i s ve ry s im i l a r t o p la in PC, ove r a
range o f f l y ash con ten ts up to 30%. Th i s i s con f i rmed by
s tud ies o f Yuan (1983) wh ich conc luded tha t t he rep lacement o f
cement w i th f l y ash has l i t t l e i n f l uence on d ry ing sh r inkage (see
f i gu re 3 .10 ) . Ch indapras i r t (2003) f ound tha t the i nco rpora t ion
o f f l y ashes reduce the d ry ing sh r inkage in compar i son w i th tha t
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3-18
o f PC. The ea r l y sh r inkage o f mor ta r w i th f i ne r f l y ash was found
to be a l i t t l e l a rge r than tha t o f the coarse r f l y ash mor ta r .
F igu re 3 .10 Dry ing sh r inkage o f conc re te inco rpo ra t i ng f l y ash
(Yuan , 1983)
3 .5 .2 .5 Creep
C reep i s de f ined as the inc rease in s t ra in (de fo rmat i on ) unde r a
sus ta ined s t ress ( l oad ) (Ho lc im, 2005) . C reep impar ts t o
conc re te a degree o f duc t i l i t y , wh ich i s des i rab le f rom the po in t
o f v iew o f s t ruc tu ra l behav iou r . However , c reep a lso has
de t r imen ta l e f fec ts on s t ruc tu res , such as inc rease de f lec t ions
wh ich can resu l t i n c rack ing , l oss o f p re -s t ress and buck l i ng o f
l ong co lumns (Add is , 2001) .
Gr i eve ’s (1991) work on concre te i nco rpora t ing f l y ash found
tha t spec i f i c c reep was reduced in f l y ash m ixes re la t i ve to p la in
m ixes w i th s im i l a r 28 -day s t reng ths . Th is con f i rms the work
done by Pandey (1983) wh ich found tha t f l y ash concre te ’s
showed l ess c reep in the ma jo r i t y o f spec imens than the
re fe rence concre te ’ s showed.
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3-19
3 .6 DURABIL ITY OF CONCRETE
Durab i l i t y may be de f ined as the ab i l i t y o f conc re te to rema in
fu l l y f unc t iona l ove r an ex tended per i od under p reva i l i ng se rv i ce
cond i t i ons fo r the pu rpose fo r wh ich i t was des igned . Concre te
w i l l rema in du rab le i f movement o f aggress i ve chemica l s w i th in
i t s s t ruc tu re i s m in im ised .
Deg rada t i on o f conc re te can be a resu l t o f t he env i ronment to
wh ich the conc re te i s exposed , o r f rom in te rna l causes w i th in
the conc re te . The ra te o f degrada t ion i s con t ro l l ed by the ra te a t
wh ich mo is tu re , a i r o r o the r aggress i ve agen ts can pene t ra te t he
conc re te . Thus cons ide r i ng the va r i ous t ranspor t mechan isms
l i ke po ros i t y and permeab i l i t y th ro ugh conc re te w i l l i nd i ca te the
in f l uence on the du rab i l i t y o f conc re te .
3 .6 .1 Poros i ty
Hardened cemen t pas tes and concre te con ta in po res o f va ry ing
t ypes and s i zes , and the re fo re the t ranspor t o f ma te r i a l s th rough
concre te can be cons ide red as the phenomenon o f f l ow th rough
a po rous med ium. The ra te o f f l ow w i l l no t on ly depend on the
poros i t y , bu t on the deg ree o f con t inu i t y o f t he pores and the i r
s i ze . A low poros i t y resu l t s i n h igh s t reng ths and l ow
permeab i l i t y i n conc re te .
The pozzo lan ic reac t ion i n f l y ash p roduces more ca lc ium
s i l i ca te hyd ra te , wh ich tends to f i l l po re spaces . F l y ash have a
l ower wa te r con ten t t han PC fo r the same workab i l i t y and as a
resu l t o f these fac to rs the poros i t y o f f l y ash concre te i s l ower
then PC.
3 .6 .2 Permeabi l i ty
Permeab i l i t y can be de f ined as the ease w i th wh ich a l i qu id o r a
gas f l ows in to ( th rough ) conc re te under a p ressure d i f f e ren t ia l
ac ross the conc re te . I t i s measured by the vo lume o f l i qu id o r
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3-20
gas t ransmi t ted pe r un i t a rea per t ime per un i t p ressure
d i f fe rence .
The ma jo r e f fec t on the pe rmeab i l i t y o f conc re te i s the cu r ing
reg ime . A i r exposure under d ry cond i t i ons i s the mos t
d i sadvan tageous . Wate r cu r ing g i ves the mos t impermeab le
conc re te . Ano the r e f fec t on the pe rmeab i l i t y o f conc re te i s the
s t ronger the conc re te and the lower the wa te r / cement ra t io ; t he
more impermeab le the conc re te .
F l y ash has the e f fec t o f reduc ing the pe rmeab i l i t y and vo lume
o f l a rge cap i l l a ry po res i n conc re te when compared w i th a p la in
CEM I conc re te o f s im i l a r s t reng th (Ba l im, 1993 ) . Th is e f fec t
d r i ves fo rm the f i neness o f the mate r ia l , t he pozzo lan ic reac t ion
and the reduced wa te r requ i rement o f the f l y ash m ixes . The
f l u id t ranspor t p roper t i es o f conc re te made w i th f l y ash a re
the re fo re cons ide rab ly reduced , thus enhanc ing the du rab i l i t y .
3 .7 ADVATAGES OF USING FLY ASH IN CONCRETE
The use o f f l y ash in conc re te has the fo l l ow ing advan tages :
• Reduc t ion in ma te r ia l cos t and the sav ing o f ene rgy by
sav ing on cement .
• Reduc t ion in bu i l d ing cos t because o f improved workab i l i t y
o f conc re te
• Be t te r wo rkab i l i t y and cohes iveness
• Reduced wa te r requ i rement fo r a g i ven s lump
• Improved impermeab i l i t y
• Reduced wa te r pene t ra t ion o f conc re te
• Reduc t ion in sh r inkage
• Improves the durab i l i t y o f conc re te i n agg ress ive
env i ronments
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3-21
3 .8 CONCLUSION
• F l y ash i s a was te ma te r i a l o f t he combus t i on o f
pu l ve r i sed coa l i n t he rma l power p l an t s . F l y ash i s us ed
i n conc re te f o r econom ic , env i r onmen ta l and du rab i l i t y
cons ide ra t i ons as a cemen t ex tende r .
• The p roduc t s o f t he pozzo lan i c r eac t i on make t he i r own
con t r i bu t i on t o t he s t r eng th and o the r p rope r t i es o f t he
cemen t and conc re te .
• The pozzo lan i c , chem ica l , phys i ca l and du rab i l i t y
p rope r t i es o f f l y ash have l ed t o i t s use as a cemen t
ex tende r i n conc re te . The p rope r t i es o f f l y ash can be
used t o i nd i ca te whe the r a gas i f i ca t i on ash i s su i t ab l e f o r
use as a cemen t ex tende r i n conc re te .
• Po r t l and cemen t pa r t i c l es a re mos t l y i n t he s i ze r ange o f
1 t o 50μm, wh i ch cause t he m ic ro f i ne pa r t i c l es o f f l y ash
t o r educe t he vo id space and co r respond ing l y t he wa te r
r equ i r emen t .
• When wo rkab i l i t y i s kep t cons tan t t he wa te r c on ten t o f a
f l y ash m ix dec reas es w i t h an i nc rease i n t he f i neness o f
t he f l y ash .
• Conc re te con ta i n i ng f l y ash shows s t r eng th ga in as a
consequence o f hea t i ng i n con t ras t o t he l oss o f s t r eng th
t ha t occu rs w i t h no rma l Po r t l and cemen t .
• The re i s a gene ra l t r end f o r t he f l exu ra l t o compress i ve
s t r eng th r a t i o t o i nc rease w i t h an i nc rease i n f l y ash
con ten t .
• The re appea rs t o be no s i gn i f i can t d i f f e rence be tween t he
modu lus o f e l as t i c i t y o f conc re te w i t h o r w i t hou t f l y ash a t
28 days .
• The rep lacemen t o f cemen t w i t h f l y ash has l i t t l e
i n f l uence on d r y i ng sh r i nkage .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
3-22
• F l y ash conc re te ’ s showed l ess c reep i n t he ma jo r i t y o f
spec imens t han t he r e fe rence conc re te ’ s showed .
• F l y ash have a l o we r wa te r con ten t t han PC fo r t he same
wo rkab i l i t y and as a r esu l t o f t hese f ac to r s t he po ros i t y o f
f l y ash conc re te i s l owe r t hen PC .
• The f l u i d t r anspo r t p rope r t i es o f conc re te made w i t h f l y
ash a re t he re fo re cons ide rab l y r educed , t hus enhanc ing
t he du rab i l i t y .
• Cons ide ra t i on o f p rope r t i es l i ke shape , pa r t i c l e s i ze ,
m ine ra l og i ca l and chem ica l compos i t i on , s t r eng th ,
e l as t i c i t y , sh r i nkage and the chem ica l r equ i r emen ts f o r
us i ng f l y ash as a cemen t e x tende r shou ld be
i nves t i ga ted when us i ng gas i f i ca t i on ash as a cemen t
ex tende r .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
4-1
4. EXPERIMENTAL PROGRAMME AND TEST PROCEDURES FOR CEMENT
4 .1 INTRODUCTION
The a im o f t h i s s tudy i s t o de te rm in e whe the r gas i f i ca t i on ash
can be used as a cemen t ex tende r i n conc re te . Cu r ren t l y
pu l ve r i sed f ue l ash (a l so ca l l ed f l y ash ) i s w ide l y used as a
cemen t ex tende r i n conc re te and t he e f f ec t o f t h i s t ype o f ash
i s we l l es tab l i shed . I n t h i s s t udy t he p rope r t i es o f cemen t and
gas i f i ca t i on ash i s exam ined t o es tab l i sh pa rame te r s f o r
cemen t b l ended w i t h gas i f i ca t i on ash .
The a im o f t h i s chap te r i s t o d i scuss t he t es t i ng me thods used
i n t he p rac t i ca l ana l ys i s o f t he r ea c t i v i t y o f a gas i f i ca t i on ash .
Pa rame te rs l i ke g r i nd i ng t ime and op t imum g yp s um con ten t was
es tab l i shed f r om the phys i ca l and chem ica l p rope r t i es o f t he
gas i f i ca t i on ash by pe r f o rm ing t es t s f o r pa r t i c l e s i ze
d i s t r i bu t i ons ; s cann ing e l ec t r on m i c roscopy pho to ’ s and x - ra y
ana l ys i s . S tanda rd t es t pe r f o rmed f o r cemen t i t i ous ma te r i a l s
w i l l be d i scussed . Tes t me thods i nc l ude t he cas t i ng and
t es t i ng o f mo r ta r p r i sms and ca lo r ime t r y t es t i ng .
4 .2 PREP AR ATION OF MATE R IALS
I n an e f f o r t t o reduce t he env i r onmen ta l impac t o f cemen t
p roduc t i on , cemen t manu fa c tu re r s a re i nc reas ing t he use o f
was te ma te r i a l s t o r ep l ace a f r ac t i on o f t he cemen t c l i n ke r .
I n t h i s p ro j ec t cemen t i s manu fac tu red i n t he l abo ra to r y us i ng
cemen t c l i n ke r ob ta i ned f r om a cemen t f ac to r y . The c l i nke r was
g round i n a ba l l m i l l ( see f i gu re 4 .1 ) w i t h 25kg o f r ound s tee l
ba l l s . The s tee l ba l l s ( s ee f i gu re 4 .2 ) we re i nd i v i dua l l y
measu red and we i ghed t o de te rm ine t he i r s i ze d i s t r i bu t i on as
i nd i ca ted i n F i gu re 4 .3 .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
4-2
F i gu re 4 .1 Labo ra to r y ba l l m i l l u sed i n expe r imen t
F i gu re 4 .2 S tee l ba l l s used f o r g r i nd i ng
A l l t he samp les g round we re s i eved t h rough a 1 .18µm s i eve
and s to red i n a i r - t i gh t con ta i ne rs .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
4-3
0
20
40
60
80
100
1 10 100
Sieve size, mm
Cum
ulat
ive
perc
enta
ge
pass
ing
%
F i gu re 4 .3 Cumu la t i ve pa r t i c l e s i ze o f s t ee l ba l l s
Cemen t and gas i f i ca t i on ash i s g round f o r d i f f e ren t t ime
i n t e r va l s t o es tab l i sh an op t imum g r i nd i ng t ime . The g r i nd i ng
t ime i n t e r va l s we re ; 30 m inu tes , 1hou r , 1hou r 30 m inu tes , 2
hou rs , 2hou r 30 m inu tes and 4hou rs . The expe r imen t i nc l uded
i n t e rb l end ing cemen t and gas i f i ca t i on ash a f t e r g r i nd i ng each
ma te r i a l sepa ra te l y , an d i n t e rg r i nd i ng o f cemen t and
gas i f i ca t i on ash by i n t e rb l end ing t he two ma te r i a l s i n t he ba l l
m i l l and g r i nd i ng i t t oge the r . No gypsum was added t o t he
cemen t c l i n ke r i n t he ba l l m i l l .
An op t imum g r i nd i ng t ime was es tab l i shed by cons ide r i ng t he
pa r t i c l e s i ze and t he f l e xu ra l and compress i ve r esu l t s o f mo r ta r
p r i sms .
The e f f ec t o f gypsum on cemen t and gas i f i ca t i on ash was
exam ined . As gypsum has a d i r ec t i n f l uence on t he se t t i ng t ime
and hea t o f hyd ra t i on an op t imum g y psum con ten t was
es tab l i shed . To de te rm ine t he op t imum gypsu m con ten t , hea t o f
hyd ra t i on cu r ves we re es tab l i shed and i so the rma l ca l o r ime t r y
t es t s we re pe r f o rmed on samp les w i t h d i f f e ren t gypsum
rep lacemen t l eve l s .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
4-4
4 .3 PHYSI CA L AND C HEMI CAL PROP ER TIES OF GASIF I C AT ION ASH
The f eed t o Saso l gas i f i e r s p r i nc i pa l l y cons i s t s o f coa rse coa l
( >5mm) and ex t r aneous rock f r agmen ts ( s t one ) . Du r i ng t he
gas i f i ca t i on o f t h i s coa rse coa l a t e l eva ted t empe ra tu res and
p ressu re a m i x tu re o f ca rbon monox ide and hyd rogen (a l so
r e fe r red t o as syn thes i s gas ) i s p roduced . The coa rse ( see
f i gu re 4 .4 ) ash i s f o rmed a t t hese e l eva ted t empe ra tu res and
p ressu re by t he i n te rac t i on o f i ne r t m ine ra l s p resen t i n t he coa l
and s tone . The coa rse ash i s r emoved f r om the gas i f i e r and
d i sposed as a by -p roduc t (Van Dyk , 2005 ) .
F i gu re 4 .4 Samp le o f gas i f i ca t i on ash c l i nke r
4 .3 .1 Pa r t i c le s i ze d is t r ibu t ion
Lase r t echno logy i s us ed t o i nves t i ga te t he pa r t i c l e s i ze
d i s t r i bu t i on o f ma te r i a l s a f t e r g r i nd i ng .
4 . 3 .1 .1 Pa r t i c l e s i ze d i s t r i bu t i on pa rame te r s
By p l o t t i ng t he i nve rse o f t he cumu la t i ve pe rcen tage
d i s t r i bu t i on , t he cumu la t i ve % ove rs i ze pa r t i c l e d i s t r i bu t i on i s
ob ta i ned . P rov i s i on was made f o r s t a t i s t i ca l ou t l i e r s by no t
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
4-5
tak i ng t he f i ve p e rcen t sma l l es t d i ame te r s and f i ve pe rce n t
l a rges t d i ame te r s i n t o accoun t .
Fo r each samp le a t r end l i ne i s added t o t he cumu la t i ve %
ove rs i ze g raph ( see f i gu re 4 .5 ) .
y = 0.9452e-0.0507x
R2 = 0.9978
0%10%20%30%40%50%60%70%80%90%
100%
0 20 40 60
Particle size (μm)
Cum
ulat
ive
% o
vers
ize
GA,2hrExpon. (GA,2hr)
F igu re 4 .5 Expon en t i a l f i t f o r cumu la t i ve % ove rs i ze pa r t i c l e
s i ze d i s t r i bu t i on
4 .3 .1 .2 Ros in -Rammle r pa r t i c l e s i ze d i s t r i bu t i on pa rame te rs
The cumu la t i ve % ove rs i ze pa r t i c l e s i ze d i s t r i bu t i on as
d i scussed i n 4 .3 .1 .1 can be rep resen ted as a Ros in -Ramml e r
d i s t r i bu t i on .
The Ros in -Ramml e r d i s t r i bu t i on g raphs (F igu re 4 .6 and F igu re
4 .7 ) a re examp le s o f how the va lues f o r t he pa r t i c l e s i ze
d i s t r i bu t i on pa rame te rs we re de r i ved . The mod i f i ed Ros in -
Rammle r d i s t r i bu t i on g raph l n l n (1 / y ) ve rsus l nx i s p l o t t ed , w i t h
y t he f i t t ed f unc t i ons y = a exp (b x ) f o r t he cumu la t i ve %
ove rs i ze pa r t i c l e s i ze d i s t r i bu t i on and x t he pa r t i c l e s i ze . A
l i nea r t r end l i ne and equa t i on i s a l so added to t hese g raphs
( see f i gu re 4 .6 ) . The s l ope and i n te r cep t i on w i t h t he ho r i zon ta l
ax i s o f t he l i ne i s t aken as t he n va lue and l n X o va lue o f t he
mod i f i ed Ros in -Rammle r f u nc t i on respec t i ve l y .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
4-6
y = 0.9665x - 2.8296R2 = 1
0
0.5
1
1.5
0 1 2 3 4 5
ln (Particle size(μm))
ln ln
(1/C
umul
ativ
e %
ov
ersi
ze)
GA,2hrLinear (GA,2hr)
F igu re 4 .6 Ros in -Rammle r d i s t r i bu t i on g raph
Slope (n) = 0.9665 Ln Xo = 2.952
Position parameter Xo = 19.14 μm
W i th t h i s ana l ys i s 36 .8% o f t he pa r t i c l es (pe r mass ) a re g rea te r
t han t he X o va lue (pos i t i on pa rame te r i n μm) . Th i s pa rame te r i s
an i nd i ca to r o f t he pa r t i c l e s i ze . The n - va lue rep resen ts t he
range o f t he pa r t i c l e s i ze d i s t r i bu t i on o f t he pa r t i c l e s i zes
g rea te r t han X o ( see f i gu re 4 .7 ) .
0%10%20%30%40%50%60%70%80%90%
100%
0 10 20 30 40 50 60
Particle size (μm)
Cum
ulat
ive
% o
vers
ize
(n) Slope indicates the range of the particle sizes greater than Xo
36.8%
Xo
F i gu re 4 .7 Exp lana t i on o f Ros in -Rammle r d i s t r i bu t i on
pa rame te rs
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
4-7
4 .3 .1 .3 Pa r t i c l e s i ze d i s t r i bu t i on pa rame te r s
The co r respond ing 50% ove rs i ze pa r t i c l e s i ze d i s t r i bu t i on i n
μm can be read f rom the exponen t i a l f i t g raph (See f i gu re 4 .8 ) .
Th i s pa r t i c l e s i ze g i ves an i nd i ca t i on o f t he ave rage pa r t i c l e
s i ze o f each samp le . I n t he same way t he 10% ove rs i ze pa r t i c l e
s i ze (D10 ) , wh i ch shows the d i f f e rence i n number o f l a rge r
pa r t i c l es i n each samp le .
y = 0.9452e-0.0507x
R2 = 0.9978
0%10%20%30%40%50%60%70%80%90%
100%
0 10 20 30 40 50 60Particle size (μm)
Cum
ulat
ive
% o
vers
ize
GA,2hrExpon. (GA,2hr)
D50 D10
F igu re 4 .8 Cumu la t i ve % ove rs i ze d i s t r i bu t i on pa rame te rs
F igu re 4 .9 i nd i ca tes t he 3 µm and the 30µm ove rs i ze pa r t i c l e s i ze
d i s t r i bu t i ons . Th i s pa r t i c l e s i ze can g i ve an i nd i ca t i on o f t he % o f t he
pa r t i c l e wh i ch l i es i n t he <3µm a nd 3 -30µm in te r va l s , wh i ch can
co r respond to t he va lues cemen t man u fac tu re r ’ s cu r ren t l y use t o l im i t
t he f i neness o f cemen t .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
4-8
y = 0.9452e-0.0507x
R2 = 0.9978
0%10%20%30%40%50%60%70%80%90%
100%
0 10 20 30 40 50 60Particle size (μm)
Cum
ulat
ive
% o
vers
ize
GA,2hrExpon. (GA,2hr)
3 µm
F igu re 4 .9 Cumu la t i ve % ove rs i ze i n te r va l s f o r 3µm and 30µm
4 .3 .2 Spec i f i c sur face a rea
A s tanda rd me thod o f de te rm in ing t he spec i f i c su r face a rea o f
cemen t wh i ch i s based on t he res i s tance t o a i r f l ow th rough a
compac t o f cemen t and was deve loped by B la ine . F igu re 4 .10
shows the appa ra tus used t o de te rm ine spec i f i c su r f ace a rea .
A cons tan t vo lume me thod whe re t he t ime , t , r equ i red t o pass a
f i xed vo lume o f a i r t h rough a compac t bed o f cemen t (12 .7 mm
d iame te r and 15 mm in dep th ) , o f s tanda rd po ros i t y i s r e l a ted
t o t he spec i f i c su r f ace o f cemen t by t he f o l l ow ing re l a t i onsh ip :
S w = K√ t ( equa t i on 4 .1 )
Where K= 281 .3915 ( cons tan t f o r appa ra tus )
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
4-9
F igu re 4 .10 Appa ra tus t o de te rm ine spec i f i c su r face a rea
4 . 3 .3 Scann ing e lec t ron mic roscop y (SEM)
A H i t ach i X -650 Scann ing E lec t ron M ic roana l yze r was used t o
t ake t he m ic rog raphs o f t he samp les . Samp les we re moun ted
on a lum in ium s tubs us ing conduc t i ve g lue and we re t hen
coa ted w i t h a t h i n l aye r o f go ld .
4 .3 .4 X - ra y f luorescence spec t roscop y (XRF)
An XRF Spec t rome te r was used to i nves t i ga te t he
cha rac te r i s t i c spec t ra o f e l emen ts p resen t i n t he so l i d samp le .
Fo r quan t i f i ca t i on ana l ys i s , t he i n tens i t y o f cha rac te r i s t i c l i ne
o f t he e lemen t ana l ysed was measu red .
The coa rse so l i d samp le was i n i t i a l l y g round to a pa r t i c l e s i ze
o f 100% <200µm. The powdered samp le was ca l c i ned a t 850 ºC
fo r 4 hou rs i n o rde r t o remo ve a l l o rgan i c compounds and wa te r
con ta ined i n t he samp le . The ca l c i ned samp le was conve r ted
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
4-10
in to a so l i d so lu t i on by f us ion w i t h l i t h i um te t ra bo ra te
(L i 2 B 4 O 7 ) . The p repa red so l i d so lu t i on and s tandard we re
p laced i n samp le ho lde rs and p laced i n t he samp le
compar tmen t o f t he XRF spec t rome te r . The i n tens i t y o f a
cha rac te r i s t i c l i ne o f t he e lemen t t o be de te rm ined was
measu red . The concen t ra t i on o f t he e lemen t i n t he samp le was
ca l cu la ted f r om the i n tens i t y measu r ed .
4 .3 .5 X - ra y d i f f rac t ion spec t roscop y (XRD)
A l l t he samp les we re rece i ved as d ry , f i ne powder . A mass o f
app rox ima te l y 4g o f each samp le , we re f u r t he r g round and
homogen i sed by hand i n an aga te mor ta r .
The add i t i ona l g r i nd ing , as requ i red f o r a quan t i t a t i ve XRD
ana l ys i s , was done us ing t he aga te segmen ts i n a McCrone
m ic ron i s ing m i l l ove r 10 m inu tes . Th i s f i ne g r i nd ing f o l l owed by
sp i k i ng t he samp les w i t h 10% (by mass ) Ca F 2 as an i n te rna l
s tanda rd , was re qu i red t o conduc t t he quan t i t a t i ve XRD
ana l yses .
App rox ima te l y 0 .5g o f t he g round samp le was p laced i n a
s ta i n l ess s tee l samp le ho lde r and exposed to t he X- ray beam
to gene ra te t he samp le ’ s d i f f r ac t i on pa t t e rn .
4 .4 STAND A RD TEST S FOR C EME NTIT IOUS MA TERIALS
F l y ash comp ly i ng w i t h t he requ i remen ts o f t he Sou th A f r i can
s tanda rd spec i f i ca t i on f o r Po r t l and cemen t ex tende rs (SANS
1491 -2 :2005 / SABS 1491 -2 :2005 ) con fo rms to t he f o l l ow ing
t es t s :
Su lphu r t r i ox i de con ten t
Loss on i gn i t i on
F ree wa te r con ten t
F ineness
Wa te r r equ i remen t
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
4-11
S t reng th Fac to r
Soundness
4 .4 .1 Su lphur t r iox ide con ten t (SANS 50 196 -2 :1994 / SABS EN 196 -2 :1994 )
1 g o f t he samp le i s we ighed ; 90m ℓ o f wa te r and 10 m ℓ o f HC I
i s added wh i l e s t i r r i ng v i go rous l y . The so lu t i on i s hea ted and
l e f t t o d i ges t j us t be low bo i l i ng po in t f o r 15 m inu tes . The
so lu t i on i s f i l t e red and washed whe re a f t e r t he so lu t i on i s
hea ted wh i l e BaC l 2 . 2H 2 O i s added to t he so lu t i on . The so lu t i on
i s d i ges ted f o r 12 hou rs and t hen f i l t e red and washed . Pape r
i s p l aced i n c ruc ib l e and p rec ip i t a te i s i gn i t ed t o cons tan t mass
a t 300°C . The su lpha te con ten t i s now de te rm ined f o r t he
samp le .
SO 3 content = (a - b ) x 34 .3 ( equa t i on 4 .2 )
c where :
a = mass o f ba r i um su lpha te f ound (g )
b = mass o f ba r i um su lpha te f ound i n b l ank de te rm ina t i on (g )
c = mass o f samp le t aken (g )
4 .4 .2 Loss on ign i t ion (SANS 5 0196 -2 :1994 / SABS EN 19 6 -2 :1994 )
We igh abou t 1g o f samp le i n to c ruc ib l e and i gn i t e a t 850°C fo r
15 m inu tes . A l l ow coo l i ng i n des i cca to r and asce r ta i n i ng
whe the r cons tan t mass i s ob ta ined by we i gh ing t he samp le .
De te rm in e t he LOI .
LOI % = (a - b ) x 100 ( equa t i on 4 .3 )
a
where :
a = mass o f samp le t aken (g )
b = mass o f r es idue (g )
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
4-12
4 .4 .3 F ree w a te r con ten t (SANS 6151 :1989 / SABS 1151 :1989 )
We igh abou t 1g o f samp le i n to c ruc ib l e and d ry t he sa mp le f o r
1 hou r i n oven a t 100°C to a cons tan t mass . A l l ow coo l i ng i n
des i cca to r and de te rm in ing t he mass o f t he d ry samp le .
Free water content % = (a - b ) x 100 ( equa t i on 4 .4 )
b where :
a = mass o f samp le (g )
b = mass o f d r i ed samp le (g )
4 .4 .4 Tes t fo r f ineness o f cement and Por t l and cement ex tenders (SANS 6 157 :2002 / SABS 1157 :2002 )
A mass o f 1 g o f t he samp le i s t aken a f t e r be ing d r i ed i n an
oven and p laced on a 45μm s ieve . The samp le i s washed w i t h
t he use o f a nozz le sp ray ing wa te r unde r a p ressu re o f 70 -
80kPa . Remo ve t he s i eve f r om und e r t he no zz le and d ry t he
s i eve w i t h t he res idue i n an oven . De te rm in e t he mass o f t he
s i eve and res idue .
Fineness, % (m/m) = c – b x 100 ( equa t i on 4 .5 )
a where :
a = d r i ed mass o f spec imen (g )
b = mass o f s i eve (g )
c = mass o f s i eve p lus res idue (g )
4 .4 .5 Wate r re qu i rement (SANS 6156 :1989 / SABS SM 115 6 :1989 )
The mor ta r was m ixed acco rd ing t o SABS Me thod 866 and the
f l ow tes t was pe r fo rmed o n t he samp le . The m ix compos i t i on
f o r mor ta r p r i sms i s seen i n Tab le 4 .1 .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
4-13
Tab le 4 .1 M ix compos i t i on f o r mor ta r p r i sms
Mater ia l Quant i ty
Wate r 225 g
Cemen t 450 g
S tanda rd re fe rence sand 1350 g
I n t h i s p ro jec t 35% o f t he cemen t wa s rep laced w i t h
gas i f i ca t i on ash as can be seen i n Tab le 4 .2 .
Tab le 4 .2 M ix compos i t i on used i n t es t
Mater ia l Quant i ty
Wate r 225 g
Gas i f i ca t i on Ash 140 g
Cemen t 310 g
S tanda rd re fe rence sand 1350 g
The f l ow tab le i s d r i ed and t he mou ld i s p l aced i n t he cen t re .
The mou ld i s ha l f - f i l l ed w i t h a l aye r o f mor ta r ( 25 mm) and
t amped 20 t imes w i t h a t amper . The mou ld i s f i l l ed and aga in
t amped 20 t imes . Excess mor ta r i s cu t o f f and mou ld i s l i f t
ve r t i ca l l y . I n a pe r i od o f 25 seconds , t he t ab le i s r a i sed and
d ropped 25 t imes t h rough a he igh t o f 12 .7 mm. A pho to o f t he
f l ow tab le t es t can be seen i n F igu re 4 .11 .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
4-14
F igu re 4 .11 Pho to o f samp le on f l ow tab le a f t e r mou ld i s
r emoved
The d iame te r o f t he mor ta r i s measu red a t f ou r app rox ima te l y
equa l - spaced i n te r va l s . The ave rage d iame te r i s ca l cu la ted and
t aken as t he f l ow . The i nc rease i n d i ame te r i s exp ressed as a
pe rcen tage o f t he o r i g i na l nom ina l d i ame te r o f t he l owe r pa r t o f
t he mor ta r spec imen (100 mm) . The d iame te r measu re men ts on
t he f l ow tab le can be seen i n t he pho to i n F igu re 4 .12 .
Ca l cu la te t o t he nea res t 1% the wa te r r equ i remen t o f t he
ma te r i a l as f o l l ows :
Water requi rement = Wt x 100 ( equa t i on 4 .6 )
Wr where :
Wt = mass o f wa te r t o p roduce f l ow va lue o f t he mor ta r t o
w i t h i n 5% po in t s o f t he re fe rence m ix (g )
Wr = ac tua l mass o f wa te r used i n re fe rence m ix (g )
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
4-15
F igu re 4 .12 Pho to o f d i ame te r measu remen ts o f f l ow tab le t es t
4 .4 .6 S t reng th fac to r t es t (SANS 50196 -1 :1994 / SABS EN 196 -1 :1994 )
The s t reng th o f cemen t can be de te rm ined by cas t i ng mor ta r
p r i sms . The spec i f i ca t i on p resc r i bes a s tanda rd m ix
compos i t i on as i nd i ca ted i n Tab le 4 .1 . The mo r ta r compos i t i on
f o r t he s t reng th t es t was as i nd i ca ted i n Tab le 4 .2 . Mor ta r was
m ixed acco rd ing t o SABS Me thod 866 . The tes t spec imens a re
40 mm x 40 mm x 160 mm p r i sms as seen i n F i gu re 4 .13 .
F i gu re 4 .13 Pho to o f mou ld used
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
4-16
The spec imens a re mou lde d a f t e r m ix i ng o f t he mor ta r . Mou lds
a re f i l l ed w i t h t he f i r s t o f two l aye rs o f mo r ta r , sp read equa l l y
i n each mou ld compar tmen t and t hen compac ted w i t h t he
v i b ra t i ng t ab le f o r 20 seconds . A f t e r compa c t i ng t he second
l aye r , t he su r face o f t he spec imen i s l eve l l ed and t he spec imen
a re cove red w i t h p l as t i c and p laced i n a cons tan t t empera tu re
room a t 22°C and 55% re la t i ve hum id i t y (RH) ove rn igh t .
Mo r ta r p r i sms a re cas t as f o r t he s t reng th f ac to r t es t ( see 4 .4 .6
s t reng th f ac to r t es t ) and t he f l ow tab le t es t ( see 4 .4 .5 ) i s
conduc ted on each d i f f e ren t mor ta r m ix . Ea ch ba tch o f mor ta r
i s m ixed mechan i ca l l y us ing a m ixe r . Ma te r i a l s a re added i n to
t he m ix i n g bow l and m ixed f o r a cons tan t t ime o f 30 seconds
whe re a f t e r t he wa te r i s added and m ixe d f o r a f u r t he r 90
seconds . Samp les a re cas t i n se t s o f t h ree p r i sms to ob ta in
s t reng ths on 2 , 7 , 28 days t o s tudy t he s t reng th deve lopmen t
ove r a l ong pe r i od .
Spec imens a re demou lded a f t e r 24 hou rs and p laced i n wa te r
a t 25 ˚C fo r cu r i ng .
F i r s t l y t he f l exu ra l s t r eng th i s de te rm i ned . P r i sms a re
suppo r ted on suppo r t s 100 mm apa r t and l oaded w i t h a po in t
l oad a t m idspan .
The f l exu ra l s t r eng th i s ca l cu la ted as f o l l ows :
R f = 1 .5 x F f x l ( equa t i on 4 .7 ) b 3
where :
R f = f l exu ra l s t r eng th (MPa)
F f = l oad app l i ed t o t he m idd le o f t he p r i sms ( kN)
l = d i s tance be tween the suppo r t s (mm)
b = s i de o f t he squa re sec t i on o f t he p r i sm (mm)
The same p r i sms tes ted i n t he f l exu ra l t es t a re t es ted f o r
compress i ve s t reng th . The two ha l ves o f each p r i sm a re t es ted
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
4-17
in t he p ress and t he ave r age o f t he s i x r esu l t s ob ta ined i s
t aken as t he compress i ve s t reng th . The compress i ve s t reng th
o f a p r i sm i s ca l cu la ted as f o l l ows :
R c = F c ( equa t i on 4 .8 )
1600
whe re :
R c = compress i ve s t reng th (MPa)
F c = ma x imum load a t f r ac tu re (N )
1600 = 40 mm x 4 0 mm, a r ea o f t he p la tens (mm)
4 .4 .7 Soundness (SANS 50196 -3 :1994 / SABS EN 196 -3 :1994 )
The pu rpose o f t h i s t es t i s t o de te rm ine t he r i s k o f expans ion
due t o hyd ra t i on . P repa re a cemen t pa s te o f s tanda rd
cons i s tency and f i l l a l i gh t l y o i l ed Le Cha te l i e r mou ld , us ing
on l y t he hands and no t v i b ra t i on . P lace t he appa ra tus i n a
hum id i t y ( 98%) cab ine t f o r 24 hou rs a t 20 °C . F igu re 4 .14
shows the Le Cha te l i e r appa ra tus i n a wa te r b a th i n a hum id i t y
cab ine t . Measu re t he d i s tance be tween the i nd i ca to r po in t s .
F i gu re 4 .14 Le Cha te l i e r mou lds i n hum id i t y cab ine t
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
4-18
Hea t mo u ld f o r 30 m inu tes and ma in ta in t he wa te r -ba th a t
bo i l i ng t empera tu re f o r t h ree hou rs . Mea su re t he d i s tance
be tween the i nd i ca to r po in t s and a l l ow mou ld t o coo l t o 20°C .
Measu re d i s tance be tween i nd i ca to r po in t s .
Soundness = c – a ( equa t i on 4 .9 )
whe re :
a = measu remen t a f t e r 24 hou rs i n hum id i t y cab ine t (mm)
c = measu remen t a f t e r coo l i ng spec imen to 20°C (mm)
4 .4 .8 Re la t i ve dens i ty (LSA Method)
The re la t i ve dens i t y o f t he samp le i s de te rm ined by :
Relat ive densi ty = c ( equa t i on 4 .10 )
(c + e ) - d where :
c = mass o f samp le (g )
d = mass o f f l ask and samp le and wa te r ( g )
e = mass o f pyknomete r and wa te r ( g )
4 .5 FACTOR S INVES T IGATE D BY CA S T ING MORTAR P R ISMS
4 .5 .1 D i f f e ren t Gr ind in g T imes
Mo r ta r p r i sms we re cas t f o r t he d i f f e ren t g r i nd ing t ime i n te r va l s
w i t h a cons tan t r ep lacemen t o f cemen t w i t h gas i f i ca t i on ash o f
35%. Mor ta r p r i sms we re wa te r cu red and compress i ve and
f l exu ra l s t r eng ths we re de te rm ined a f t e r 2 , 7 and 28 days . The
m ix comp os i t i on f o r bo th i n te rb lend ing cemen t and gas i f i ca t i on
ash a f t e r g r i nd ing each ma te r i a l sepa ra te l y , and i n te rg r i nd ing
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
4-19
o f cemen t and gas i f i ca t i on ash by i n te rb lend ing t he two
ma te r i a l s i n t he ba l l m i l l and g r i nd ing i t t oge the r i s seen i n
Tab le 4 .3 and Tab le 4 .4 . The gypsum con ten t was cons tan t a t
2 .5% rep lacemen t o f t he cemen t con ten t .
Tab le 4 .3 Mor ta r p r i sm m ix co mpos i t i on f o r i n te rb lend ing
cemen t and Gas i f i ca t i on ash
Material Mass (g) Cement 292.5 Gasification ash 157.5 Gypsum 7.31 Water 225 Standard reference sand 1350
Tab le 4 .4 Mor ta r p r i sm m ix compos i t i on f o r i n te rg r i nd ing
cemen t and Gas i f i ca t i on ash
Material Mass (g)
Cement and Gasification ash interground 450
Gypsum 7.31
Water 225
Standard reference sand 1350
4 .5 .2 D i f f e ren t Gypsum Percen tages
Mo r ta r p r i sms we re cas t f o r i n t he ba l l m i l l t o t es t t he e f f ec t o f
d i f f e ren t gypsum pe rcen tages and t o es tab l i sh t he d i f f e rence
be tween the l abo ra to ry i n te rb lended and i n te rg round cemen ts
w i t h a commerc ia l l y ava i l ab le CEM I 42 .5 . Tab le 4 .5 shows the
d i f f e ren t we igh t s f o r gypsum as a pe rcen tage o f t he cemen t
con ten t .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
4-20
Tab le 4 .5 Gypsum rep lacemen t we igh t s f o r mor ta r p r i sms
Gypsum replacement %
Gypsum content (g)
0.0% 0.00 0.5% 1.46 1.0% 2.93 1.5% 4.39 2.0% 5.85 2.5% 7.31 3.0% 8.78
4 . 5 .3 I so therma l Conduc t ion Ca lo r imet ry
I n i so the rma l conduc t i on ca lo r ime t r y , t he hea t o f hyd ra t i on o f
cemen t i s d i r ec t l y measu red by mon i t o r i ng t he hea t f l ow f rom
the spec imen when bo th t he spec imen and the su r round ing
env i ronmen t a re ma in ta ined a t app rox ima te l y i so the rma l
cond i t i ons . App rox ima te l y 3g o f wa te r we re i nocu la ted i n to an
equ i va len t mass o f r eac tan t powder t ha t had been p laced i n a
coppe r samp le cup and p laced w i t h i n t he ca lo r ime t r y cav i t y .
The cups we re se a led w i t h p l as t i c f i lm t o m in im ize eva po ra t i on
o f wa te r . Each reac tan t was a l l owed to equ i l i b ra te sepa ra te l y
t o 25 ºC , p r i o r t o m i x i ng . The wa te r was equ i l i b ra ted i n a
sy r i nge and when equ i l i b r i um had been ach ieved the p las t i c
f i lm was pene t ra ted and t he wa te r i n j ec ted ove r t he so l i ds . The
ra tes o f hea t evo lu t i on , dQ/d t i n mW/g we re measu red and
reco rded us ing a compu te r da ta acqu i s i t i on sys tem.
The hea t o f hyd ra t i on o f a mor ta r m ix was a l so i nves t i ga ted .
Mor ta r m ixes we re m ixe d and cas t i n to a s tee l cy l i nde r .
The rmocoup les we re i nse r ted i n to t he pocke t o f t he s tee l
cy l i nde rs ’ l i d . The cy l i nde r and t he rmocoup le we re p laced i n to
a t empera tu re i so la t i on f l ask and l e f t i n a cons tan t t empera tu re
room a t 25 ºC .
The t he rmocoup les reco rded the t empera tu re o f t he mor ta r ove r
112 hou rs . A f t e rwa rds t he t he rmocoup les we re removed and
t he da ta we re down loaded w i t h a compu te r sys tem.
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
4-21
4 .5 .3 D i f f e ren t rep lacements percen tages o f Gas i f i ca t ion Ash
Mor ta r p r i sms we re cas t f o r d i f f e ren t r ep lacemen t pe r cen tages
o f Gas i f i ca t i on ash . Gas i f i ca t i on ash we re rep laced i n t he ba l l
m i l l and g rounded w i t h cemen t . These rep lacemen t pe rcen tages
we re : 0%, 10%, 20%, 35% and 55%. The rep lacemen t
pe rcen tages we re se lec ted as t he h ighes t i n te r va l cu r ren t l y
used i n commerc ia l l y ava i l ab le CEM I ( 0%) , CEM I I ( 6 - 10% and
21 -35%) and CEM IV (36 -55%) .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
5-1
5. EXPERIMENTAL PROGRAMME AND TEST PROCEDURES FOR CONCRETE
5 . 1 INTRODUCTION
The a im o f t h i s s tudy i s t o de te rm in e whe the r gas i f i ca t i on ash
can be used as a cemen t ex tende r i n conc re te . Cu r ren t l y
pu l ve r i sed f ue l ash (a l so ca l l ed f l y ash ) i s w ide l y used as a
cemen t ex tende r i n conc re te and t he e f f ec t o f t h i s t ype o f ash
i s we l l es tab l i shed . I n t h i s s t udy t he p rope r t i es o f cemen t and
conc re te con ta i n ing gas i f i ca t i on ash w i l l be compa red t o t he
p rope r t i es o f cemen t and conc re te con ta i n i ng f l y ash .
The a im o f t h i s chap te r i s t o d i scuss t he t es t i ng me thods used
i n t he p rac t i ca l ana l ys i s o f t he r eac t i v i t y o f a gas i f i ca t i on ash .
The m ix des ign f o r d i f f e ren t m i xes o f conc re te w i l l be
d i scussed . The t es t i ng o f conc re te cubes , c y l i nde rs and
sh r i nkage beams w i l l be d i scussed w i t h r e fe rence t o t he t es t i ng
appa ra tus , as we l l as t he s tanda rd i sed t es t i ng me thods used .
5 .2 M IX DESI GN FOR CONCRE TE MIXE S
Conc re te was ba t ched f o r t h ree d i f f e ren t m i xes t o i nves t i ga te
cube s t r eng ths , t ens i l e s t r eng ths , E - va lues , sh r i nkage , c reep ,
po ros i t y and pe rmeab i l i t y .
Each m ix ( see Tab le 5 .1 ) had a wa te r / cemen t r a t i o o f 0 . 6 . The
agg rega te con ten t was ma de up o f do l om i t e sand and 1 /3 o f
9 . 5mm a nd 2 /3 19mm g ra n i t e s t one . A 35% subs t i t u t i on o f
cemen t i t i ous ma te r i a l s was cons ide red whe re app l i cab le f o r t he
m i xes . Th e s i ze o f t he m i xes was 43 ℓ .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
5-2
Tab le 5 .1 M i x compos i t i on fo r conc re te m i xes
Mater ia ls Quant i t y 43ℓ Pe r kg /m³
Wate r 9 ℓ 210 ℓ
Cement 9 .8 kg 227 kg
Cement i t ious mate r ia l 5 . 3 kg 123 kg
Do lomi te Sand 37 .7 kg 875 kg
9 .5mm Gran i te S tone 14 .2 kg 330 kg
19mm Gran i te S tone 28 .4 kg 660 kg
The m ix compos i t i on r ema ined cons tan t and on l y t he t ype o f
cemen t i t i ous ma te r i a l used was changed . The cemen t used i n
t he m i xes can be seen i n Tab le 5 .2 .
Tab le 5 .2 Conc re te m i x compos i t i on
Mix Descr ip t ion Abbrev ia t ion
Mix 1 In te rg r in d ing o f cement and gas i f i ca t ion ash IG
M ix 2 In te rb lend ing o f cement and gas i f i ca t ion ash IB GA
Mix 3 In te rb lend ing o f cement and f l y ash IB FA
5 .3 TEST CONDUCTE D ON F R ESH CONCRETE MIXES
5 .3 .1 S lump Tes t (SANS 586 / SABS SM 82 :1994 )
The s l ump t es t i s a me thod t o meas u re t he cons i s t ency o f t h e
conc re te . I t does howeve r no t t es t a l l t he cons i s t ency
r equ i r emen ts and has a l im i t ed app l i ca t i on .
I n t he s l ump t es t t he mo u ld i s f i l l ed i n t h ree equa l l a ye rs ,
sub jec t i ng each l aye r t o 25 b l ows f r om the tamp ing rod wh i l e
t he mou ld i s f i rm l y he ld down by s tand ing on t he f oo t p i eces .
The su r f ace i s smoo thed , t he cone i s r emo ved and t he s l ump i s
measu red t o t he nea res t 5 mm. The s l ump i s t he d i s t ance
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
5-3
be tween t he t op o f t he i nve r t ed mou ld and t he h i ghes t po in t o f
t he conc re te as i nd i ca ted i n F i gu re 5 .1 .
F i gu re 5 .1 Measu r i ng t he s l ump (Add i s , 2001 )
5 .4 STRENGTH TEST S
5 .4 .1 Compres s ive S t reng th Tes t (SANS 5863 -1 /SABS 863 -1994 )
Tes t spec imens a re c rushed be tween two p l a tens i n a hyd rau l i c
p ress . The ra te o f l oad app l i ca t i on i n f l uences t he compress i ve
s t r eng th r esu l t s and i s spec i f i ed a t a un i f o rm ra te o f 0 . 3 MPa /s
± 0 .1 MPa /s .
A l l t he cubes we re wa te r cu red . Th ree cubes (100x100x100 )
f r om each m ix we re c rushed on 2 , 7 and 28 days and t he
ave rage o f t he t h ree cube s t r eng ths was de f i ned as the
s t r eng th . The compress i ve s t r eng th i s r eco rded t o t he nea res t
0 .5MPa .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
5-4
5 .4 .2 Sp l i t t ing Cy l inder Tes t fo r Tens i l e S t reng th (SANS 625 :1994 /SABS SM 1253 :1994 )
I n Sou th A f r i ca t he t ens i l e s t r eng th o f conc re te i s de te rm ined
i nd i r ec t l y by b reak ing beam spec imens i n f l e xu re o r by sp l i t t i ng
cy l i nde rs by app l y i ng l i ne l oads .
The cy l i nde r i s p l aced w i th i t s ax i s ho r i zon ta l be tween t he
p l a tens o f t he t es t i ng mach ine , and t he l oad i s i nc reased un t i l
f a i l u re occu rs by i nd i r ec t t ens i on i n t he f o rm o f sp l i t t i ng a l ong
t he ve r t i ca l p l ane t akes p l ace . Fo r each m ix , two cy l i nd r i ca l
samp les we re sp l i t .
The f o l l ow ing equa t i on was app l i ed t o de te rm ine t he t ens i l e
s t r eng th o f t he conc re te acco rd i ng to t he e l as t i c t heo ry :
f = 2 x P ( equa t i on 5 .1 )
πdℓ
whe re :
f = t ens i l e s t r eng th (MPa)
P = compress ion l oad a t f a i l u re (N )
d = d i ame te r o f c y l i nde r (mm)
ℓ = l eng th o f c y l i nde r (mm)
A l l t he cy l i nde rs we re wa te r cu red and two cy l i nde rs f r om each
m ix we re used t o de te rm ine t he t ens i l e s t r eng th .
5 .5 DEFORMATION A ND V OLU ME C HA NGE OF CON CRE TE
5 .5 .1 E -Va lue Tes t
De fo rma t i on t akes p l ace when a l oad i s app l i ed t o a s t r uc tu ra l
ma te r i a l . I f t he r a t i o o f t he app l i ed compress i ve s t r eng th t o t he
l ong i t ud i na l s t r a i n p roduced i s cons tan t , t he cons tan t i s ca l l ed
t he modu lus o f e l as t i c i t y (Young ’ s modu lus ) .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
5-5
The non - l i nea r i t y o f t he s t ress - s t r a i n r e l a t i onsh ip f o r conc re te
i s ma in l y due t o t he non - l i nea r s t r ess - s t r a i n r esponse o f t he
pas te . A po r t i on o f t he cu r ve may be rega rded as be ing
e f f ec t i ve l y l i nea r , and a t s t r esses w i t h i n t h i s r ange t he e l as t i c
modu lus may be t aken as t he s l ope o f t he l i nea r po r t i on . Fo r
t h i s po r t i on Hooke ’ s l aw may be used t o de te rm ine t he modu lus
o f e l as t i c i t y .
The re i s no SABS tes t me thod t o de te rm ine t he s ta t i c e l as t i c
modu lus o f conc re te and t he re fo re ASTM C 4 69 -02 i s used . The
t es t s de te rm ine i n i t i a l t angen t mod u lus (Young ’ s ) as we l l as
t he secan t modu lus co r respond ing t o one t h i r d o f t he
compress i ve f a i l u re s t r ess . The t es t i n vo l ves l oad ing a cy l i nde r
a t a cons tan t r a t e and reco rd i ng t he l oad ( s t r ess ) and
de fo rma t i on ( s t r a i n ) o f t he spec imen . A s t r ess - s t r a i n cu r ve i s
de te rm ined f r om wh i ch t he modu lus o f e l as t i c i t y i s de te rm ined .
The modu lus o f e l as t i c i t y was de te rm ined as f o l l ows :
∆L = G L – G F ( equa t i on 5 .2 )
2
ε = ∆L ( equa t i on 5 .3 )
L
P = (P L – P F ) x 1000 ( equa t i on 5 .4 )
A = πd 2 ( equa t i on 5 .5 )
4
σ = P ( equa t i on 5 .6 )
A
E = σ ( equa t i on 5 .7 )
ε
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
5-6
whe re :
G L = Las t r ead ing o f gauge (µm)
G f = F i r s t r ead ing o f gauge (µm)
L = d i s t ance be tween measu r i ng po in t s (mm)
P L = l as t s t r eng th i n t e r va l ( kN )
P F = f i r s t s t r eng th i n t e r va l ( kN )
d = d i ame te r o f c y l i nde r (mm)
E = s ta t i c modu lus o f e l as t i c i t y (GPa)
Cy l i nde rs we re wa te r cu red f o r 28 days . Fo r t he de te rm ina t i on
o f t he modu lus o f e l as t i c i t y , two cy l i nde rs o f each m ix we re
t es ted a f t e r t he 28 -day compress i ve r esu l t s o f t he cubes we re
de te rm ined .
5 .5 .2 Shr inkage and Creep Tes t (ASTM C 512 -02 )
Vo lume change occu rs i n conc re te i n bo th t he f r esh and
ha rdened s ta te . S t r uc tu ra l pe r f o rma nce i s mos t conce rned by
t he vo l ume change assoc ia ted w i t h an i n t e r change o f mo i s tu re
be tween ha rdened conc re te and t he env i r onmen t .
Swe l l i ng occu rs when t he ne t f l ow o f mo i s tu re f r om the
env i r onmen t t o t he conc re te cause a vo l ume i nc rease and
sh r i nkage occu rs when a n e t ou t f l ow f r om t he conc re te t o t he
env i r onmen t r esu l t s i n a dec rease i n vo l ume . Con ven t i ona l
conc re te usua l l y con ta i ns mo re wa te r t han wha t can be
chem ica l l y comb ined w i t h t he cemen t and t he re i s a t endency
f o r mo i s tu re t o be l os t f r om the conc re te , r esu l t i ng i n
sh r i nkage .
C reep i s de f i ned as t he i nc rease i n s t r a i n ( de fo rma t i on ) unde r
a sus ta i ned s t r ess ( l oad ) . When l oaded , conc re te expe r i ences
an i ns tan taneous e l as t i c s t r a i n , wh i ch i s r ecove rab le . I n
add i t i on , an i ne l as t i c c reep s t r a i n t akes p l ace t ha t i s on l y
pa r t i a l l y r ecove rab le .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
5-7
Sh r i nkage i s t es ted i n con junc t i on w i t h c reep . Th ree cy l i nde rs
we re cas t and cu red i n wa te r f o r 28 days . Fo r t he t es t , one
cy l i nde r i s used f o r sh r i nkage and two cy l i nde rs fo r c reep
t es t i ng . The sh r i nkage t es t i s a na tu ra l d ry i ng me thod whe re
t he cy l i nde r i s d r i ed i n a con t ro l l ed env i r onmen t o f 65±5%
re l a t i ve hum id i t y and 22 ±2 ºC . Th e sh r i nkage mo vemen t i s
measu red ove r a pe r i od o f t ime .
The t es t me thod f o r c reep measu res t he l oad - i nduced t ime
dependen t compress i ve s t ra i n a t se l ec ted ages f o r conc re te .
The cube compress i ve s t r eng ths o f t he d i f f e ren t m i xes a re
de te rm ined on 28 days . The cy l i nd r i ca l samp les a re p l aced i n t o
a l oad ing f r ame a nd l oaded w i t h 40% o f t he compress i ve l oad .
S t ra i n r ead ings a re t aken immed ia te l y be fo re and a f t e r l oad ing ,
and t he rea f t e r a t r egu la r t ime i n t e r va l s .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
5-8
F i gu re 5 .2 Pho to o f l ab se t - up f o r measu r i ng sh r i nkage and
c reep
5 .6 DUR ABIL ITY
Durab i l i t y can be de f i ned as , “ t he capab i l i t y o f ma in ta i n i ng t he
se r v i ceab i l i t y o f a p roduc t , componen t assemb ly o r cons t ruc t i on
ove r a spec i f i ed t ime ” .
The qua l i t y o f conc re te canno t be de te rm ined by on l y u s i ng t he
s t r eng th t es t as th i s app roach does no t g i ve an adequa te
i nd i ca t i on o f t he qua l i t y o f t he cove r conc re te . The cove r
conc re te ac t s as a ba r r i e r be tween t he r e i n fo r c i ng s t ee l and
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
5-9
the ex te rna l agg ress i ve env i r onmen t and i t s qua l i t y i s o f g rea t
impo r t ance i n du rab i l i t y cons ide ra t i ons .
The du rab i l i t y o f conc re te i s a f unc t i on o f po ros i t y . S t r eng th
i nc reases w i t h dec reas ing po ros i t y and po ros i t y i s a f f ec ted by
cap i l l a r y po ros i t y and a i r - vo i d po ros i t y . Po ros i t y may be
de f i ned as t he pe rcen tage vo ids i n a samp le . Vo ids , wh i ch a re
spaces f i l l ed w i t h wa te r , a re a r esu l t o f t he fa i l u re t o expe l a l l
t he a i r f r om the we t conc re te .
The me t hod t ha t has been adop ted i s t o measu re a f l u i d
t r anspo r t pa rame te r o f t he ma te r i a l such as pe rmeab i l i t y t o
l i qu i ds o r gasses . F l u i d t r anspo r t p rope r t i es a re i n f l uenced by
cap i l l a r y po ros i t y and t he deg ree o f i n t e r connec t i on cap i l l a r i es .
Pe rmeab i l i t y ma y be de f i ned as t he ease w i t h wh i ch a l i qu i d o r
gas can pass t h rough a spec i f i c ma te r i a l .
5 . 6 .1 Poros i ty Tes t
Fo r each o f t he t h ree m ixes , two wa te r - cu red samp les we re
t es ted a f t e r 28 days . A co re was d r i l l ed f r om 150x1 50 cubes
and oven -d r i ed a t a t emp e ra tu re o f 100 ˚C fo r 24 hou rs t o
ensu re tha t a l l mo i s t u re was removed . A f t e r de te rm in i ng t he
we igh t o f t he oven -d r i ed samp les , t hey we re p l aced i n a
vacuum f o r 24 hou rs . The samp les we re t hen submerged i n de -
a i r ed d i s t i l l ed wa te r and once aga in p l aced i n a vacuum fo r 3
hou rs . Th i s was done t o ensu re t ha t a l l t he vo i ds i n t he
conc re te samp les we re f i l l ed w i t h wa te r . F ina l l y t he
submerged we igh t o f t he samp les wa s de te rm ined . The po ros i t y
t es t se t up can be seen i n F i gu re 5 .3 .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
5-10
F igu re 5 .3 Pho to o f po ros i t y t es t se t up
The f o l l ow ing equa t i on was app l i ed to de te rm ine t he po ros i t y o f
t he conc re te :
Porosi ty = mass s a t – mass d r y ( equa t i on 5 .8 )
mass s a t – mass w a t
whe re :
mass s a t = we igh t o f sa tu ra ted samp le ( g )
mass d r y = we igh t o f oven -d r i ed samp le ( g )
mass w a t = we igh t o f samp le i n wa te r ( g )
5 .6 .2 Ox ygen Permeab i l i t y Tes t
The oxyg en pe rme ab i l i t y o f t he conc re te was de te rm ined f o r
two samp les o f each m ix a f t e r 28 days . A co re was d r i l l ed f r om
the 150x150 cube and oven -d r i ed a t 100 ˚C fo r 24 hou rs t o
p reven t expans ion c racks , wh i ch wou ld i n f l uence t he
pe rmeab i l i t y r ead ings . The appa ra tus cons i s t s o f a se r i es o f
va l ves , wh i ch de l i ve red o x ygen a t a known p ressu re t h rough
t he samp les , and ca l i b ra ted g l ass tubes t h rough wh i ch t he r a te
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
5-11
a t wh i ch t he oxyg en bubb les moved cou ld be measu red w i t h a
s t opwa tch .
The f o l l ow ing equa t i on was app l i ed t o de te rm ine t he
pe rmeab i l i t y coe f f i c i en t , k , o f t he conc re te .
K = 2 x t x Q x e x P ( equa t i on 5 .9 )
A (P 22 – P 1
2 )
whe re :
t = samp le t h i c kness (m)
e = oxyg en v i s c os i t y ( 2 .02 - 5 N . s /m 2 )
K = oxygen pe rmeab i l i t y ( l /m 2 )
Q = vo lu me pe r second pass ing t h rough samp le (m /s ³ )
A = c ross sec t i ona l a rea o f samp le (m 2 )
P 1 = a tmosphe r i c p ressu re (Pa )
P 2 = app l i ed p ressu re (Pa )
The oxyg en pe rmeab i l i t y i ndex (OP I ) can be ca l cu l a ted as :
OPI = -L og 1 0 K ( equa t i on 5 .10 )
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-1
6. TEST RESULTS AND DISCUSSION ON CEMENT TESTS
6 .1 INTRODUCTION
I n chap te r 6 , t he r esu l t s o f t he expe r imen ta l t es t s d i scussed i n
chap te r 4 a re r ev i ewed and ana l ysed t o examine t he reac t i v i t y
o f a gas i f i ca t i on as h used as a cemen t ex tende r .
F i r s t l y t he phys i ca l p rope r t i es o f t he gas i f i c a t i on ash w i l l be
d i scussed w i t h r e fe rence to t he pa r t i c l e s i ze d i s t r i bu t i on and
t he shape o f t he pa r t i c l es . The chem ica l p rope r t i es o f t he
gas i f i ca t i on ash w i l l be ana l ysed by cons ide r i ng t he r esu l t s
f r om XRF , XRD an d s tanda rd t es t s f o r ex tende rs .
The rea f t e r t he resu l t s o f t he mor ta r p r i sm resu l t s f o r i n t e r va l s
o f g r i nd i ng t imes and d i f f e ren t gypsum pe rcen tages w i l l be
i l l u s t r a ted and d i scussed . The d i scuss i on o f t he r esu l t s t akes
i n t o cons ide ra t i on t ha t t es t s we re conduc ted on a s i ng l e se t o f
samp les . L im i t a t i ons t o t he t es t i ng me thod w i l l be d i scussed
and poss ib l e imp rovemen ts w i l l be r ecommend ed .
6 .2 PHYSI CAL PROP E RTIES
6 .2 .1 Pa r t i c le S i ze D is t r ibu t ion Tes t
The wa te r dema nd and wo rkab i l i t y o f cemen t pas te i s
con t ro l l ed by t he pa r t i c l e s i ze d i s t r i bu t i on . As no th i ng can be
done t o a l t e r t he m ine ra l og i ca l cha rac te r i s t i c s , t he con t ro l o f
pa r t i c l e s i ze d i s t r i bu t i on i s t he on l y p rac t i ca l me thod by wh i ch
t he cemen t i t i ous ac t i v i t y can be enhanced .
The pa r t i c l e s i ze d i s t r i bu t i on o f t he cemen t and gas i f i ca t i on
ash g round f o r a two hou r t ime i n t e r va l can be seen i n F i gu re
6 .1 . I t i s obse rved t ha t t he gas i f i ca t i on ash , g r i nded sepa ra te
and i n t e rg round w i t h cemen t had s im i l a r pa r t i c l e s i ze
d i s t r i bu t i ons . The re i s a cons ide rab le d i f f e renc e i n pa r t i c l e s i ze
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-2
be tween t he gas i f i ca t i on ash and cemen t g r i nded sepa ra te l y f o r
t he same t ime i n t e r va l . The gas i f i ca t i on ash had a pa r t i c l e s i ze
r ange be tween 0 .08 μm and 50μm, whe re t he cemen t pa r t i c l es
r anged be tween 2μm and 110 μm. The resu l t s f o r a l l t he
g r i nd i ng t ime i n t e r va l s can be seen i n Append i x A . These
resu l t s i nd i ca te tha t t he cemen t c l i n ke r i s ha rde r t han t he
gas i f i ca t i on ash c l i n ke r . The pa r t i c l e s i ze o f i n t e rg r i nd i ng 65%
cemen t and 35% gas i f i ca t i on ash shows t ha t t he pa r t i c l e s i ze
d i s t r i bu t i on f o r t ime i n t e r va l s 1 ,5 hou rs and 2 hou rs we re
i den t i ca l . Fu r t he r g r i nd i ng d i d no t r educe t he f i neness o f t he
i n t e rg round samp le s i gn i f i can t l y ( see F igu re 6 .2 ) . Thus f r om
the pa r t i c l e s i ze d i s t r i bu t i on i t i s c l ea r t ha t an op t imum
g r i nd i ng t ime can be es tab l i shed .
H ighe r f i neness p rov i des a g rea te r su r f ace a rea t o be we t t ed ,
r esu l t i ng i n an acce le ra t i on o f t he hyd ra t i on r eac t i on . I t was
t hus expec ted t ha t t he sma l l e r pa r t i c l e s i ze o f t he gas i f i ca t i on
ash shou ld r equ i r e t he same o r mo re wa te r t han f l y ash .
0
10
20
30
40
50
60
70
80
90
100
0.01 0.1 1 10 100 1000
Particle size (μm)
Cum
ulat
ive
part
icle
siz
e %
IG,2hrGA,2hrCEM,2hrFly ash
F i gu re 6 .1 G raph o f cumu la t i ve pa r t i c l e s i ze d i s t r i bu t i on o f
cemen t and gas i f i ca t i on ash (g r i nded sepa ra te and i n te rg round )
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-3
0102030405060708090
100
0.1 1 10 100 1000
Particle size (μm)
Cum
ulat
ive
part
icle
siz
e %
IG, 30min
IG,1hr
IG,1.5hr
IG,2hrIG,2.5hr
IG,4hr
F i gu re 6 .2 Cumu l a t i ve pa r t i c l e s i zes f o r gas i f i ca t i on ash and
cemen t i n t e rg round
The re l evance o f t he Ros in -Ramml e r pa r t i c l e s i ze d i s t r i bu t i on
pa rame te r s was eva lua ted by compa r i ng t he f i t t ed f unc t i ons f o r
t he cumu la t i ve % ove rs i ze pa r t i c l e s i ze d i s t r i bu t i ons f o r
d i f f e ren t g r i nd i ng t imes . Bo th t he cons tan ts i n t he equa t i on
va r y w i t h g r i nd i ng t ime an d t he re fo re t he cons tan t s as such
canno t be used t o compa re t he samp les (See t ab l e 6 .1 ) . The
f unc t i ons f o r gas i f i ca t i on ash a re p l o t t ed i n F i gu re 6 .3 . The res t
o f t he pa r t i c l e s i ze d i s t r i bu t i ons can be v i ewed i n Append i x B .
0%10%20%30%40%50%60%70%80%90%
100%
0 50 100 150 200 250
Particle size (μm)
Cum
ulat
ive
% o
vers
ize
GA,30minGA,1hrGA,1.5hrGA,2hrGA,2.5hrGA,4hr
F igu re 6 .3 Summary o f e xponen t i a l f i t t ed f unc t i ons f o r t he
cumu la t i ve % ove rs i ze pa r t i c l e s i ze d i s t r i bu t i on
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-4
Acco rd i ng t o F i gu re 6 .3 t he pos i t i on pa rame te r (X o ) and
t he re fo re t he pa r t i c l e s i ze d i s t r i bu t i on dec rease as t he g r i nd i ng
t ime i nc reases f o r gas i f i ca t i on ash . I t i s c l ea r t ha t t he g r i nd i ng
t ime has a s i gn i f i can t i n f l uence on t he range o f t he pa r t i c l e
s i ze d i s t r i bu t i ons g rea te r t han t he pos i t i on pa rame te r ( X o ) . The
sho r t e r g r i nd i ng t imes seem to have more o f t he l a rge r ( coa rse )
pa r t i c l es . Th i s t r end can a l so be seen when compa r i ng t he
Ros in -Rammle r s l ope (n ) pa rame te r s ( see F igu re 6 .4 ) . See
Append i x C f o r r es t o f g raphs .
The g raph c l ea r l y i nd i ca tes t ha t t he pa r t i c l e s i ze o f gas i f i ca t i on
ash dec reases as t he g r i nd i ng t ime i nc rease . The f i t t ed t r end
l i ne t ha t bes t desc r i bes t he measu red va lues i s an exponen t i a l
f unc t i on . The s ta t i s t i ca l R -squa re va lue f o r a l l t he samp les o f
t he expo nen t i a l f i t i s be tween 0 .995 and 0 .999 . The exponen t i a l
equa t i on i s t he re fo re a t r ue r ep resen ta t i ve o f t he cumu la t i ve %
ove rs i ze pa r t i c l e s i ze d i s t r i bu t i on .
0
0.5
1
1.5
0 1 2 3 4 5 6
ln (Particle size (μm))
ln ln
(1/c
umul
ativ
e %
ov
ersi
ze)
GA,30minGA,1hrGA,1.5hrGA,2hrGA,2.5hrGA,4hr
F i gu re 6 .4 Summa ry o f Ros in -Rammle r d i s t r i bu t i ons
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-5
Tab le 6 .1 F i t t ed f unc t i ons o f ove rs i ze pa r t i c l e s i ze d i s t r i bu t i on
Fitted function
y = a e(bx) Sample
a b
R² Xo
IG,30 min 0.955 -0.0198 0.9996 47.90
IG,1hr 0.975 -0.0354 0.9997 28.01
IG, 1.5hr 0.9929 -0.0514 0.998 19.88
IG, 2hr 0.9835 -0.05 0.9983 20.00
IG, 2.5hr 0.9693 -0.0532 0.9986 18.20
IG, 4hr 0.9822 -0.0608 0.9963 16.69
GA,30min 0.9429 -0.0122 0.9991 78.35
GA, 1hr 0.9329 -0.0284 0.9989 33.05
GA, 1.5hr 0.9331 -0.0382 0.9986 24.51
GA, 2hr 0.9452 -0.0507 0.9978 19.14
GA, 2.5hr 0.9254 -0.0554 0.9981 16.64
GA, 4hr 0.8942 -0.0781 0.9952 10.93
Cem,30min 0.9675 -0.024 0.9936 37.71
Cem, 1hr 0.7121 -0.0144 0.8842 33.11
Cem, 1.5hr 0.9411 -0.0249 0.9858 37.29
Cem, 2hr 0.8794 -0.0237 0.9681 29.43
Cem, 2.5hr 0.9077 -0.0247 0.9791 32.04
Cem, 4hr 0.8179 -0.0179 0.9454 25.71
IB, 30 min 0.9031 -0.0165 0.9874 45.51
IB, 1hr 0.8898 -0.023 0.9792 31.66
IB, 1.5hr 0.9607 -0.03 0.9973 30.55
IB, 2hr 0.945 -0.033 0.9946 25.93
IB, 2.5hr 0.9142 -0.0321 0.9897 25.59
IB, 4hr 0.8079 -0.0256 0.9545 23.27
The va lues o f t he s l ope n and t he pos i t i on pa rame te r X o f o r a l l
t he samp les can be seen i n Tab le 6 .2 . The equa t i ons f o r t he
l i nea r t r end l i ne f i t t ed t o t he Ros in -Rammle r d i s t r i bu t i on g raph
and t he s ta t i s t i ca l R -squa re va lue o f t he l i nea r f i t a re a l so
l i s t ed i n Tab le 6 .2 .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-6
Tab le 6 .2 Ros in -Rammle r p a r t i c l e s i ze d i s t r i bu t i on pa rame te r s
Fitted function
y = cx +d Sample
c d
R² Xo n
IG,30 min 0.9743 -3.7795 1 47.90 0.9743
IG,1hr 0.9848 -3.2664 1 28.01 0.9848
IG, 1.5hr 0.9959 -2.9494 1 19.88 0.9959
IG, 2hr 0.9902 -2.951 1 20.00 0.9902
IG, 2.5hr 0.9813 -2.8498 1 18.20 0.9813
IG, 4hr 0.9896 -2.7544 1 16.69 0.9896
GA,30min 0.9653 -4.0996 1 78.35 0.9653
GA, 1hr 0.958 -3.347 1 33.05 0.958
GA, 1.5hr 0.9589 -3.0666 1 24.51 0.9589
GA, 2hr 0.9665 -2.8296 1 19.14 0.9665
GA, 2.5hr 0.9543 -2.6897 1 16.64 0.9543
GA, 4hr 0.934 -2.2793 0.9999 10.93 0.934
Cem,30min 0.9816 -3.6309 1 37.71 0.9816
Cem, 1hr 0.816 -3.1629 0.9984 33.11 0.816
Cem, 1.5hr 0.9662 -3.5129 1 37.29 0.9662
Cem, 2hr 0.9307 -3.3684 0.9999 29.43 0.9307
Cem, 2.5hr 0.9469 -3.4172 0.9999 32.04 0.9469
Cem, 4hr 0.8908 -3.4053 0.9996 25.71 0.8908
IB, 30 min 0.9424 -3.7753 0.9999 45.51 0.9424
IB, 1hr 0.9348 -3.4207 0.9999 31.66 0.9348
IB, 1.5hr 0.9777 -3.3921 1 30.55 0.9777
IB, 2hr 0.9686 -3.2527 1 25.93 0.9686
IB, 2.5hr 0.9499 -2.0479 0.9999 25.59 0.9499
IB, 4hr 0.8839 -3.0507 0.9995 23.27 0.8839
The e f f ec t o f g r i nd i ng t ime on pa r t i c l e s i ze d i s t r i bu t i on can be
seen i n F i gu re 6 .5 . F rom t he g raph i t i s obse rved t ha t as t he
g r i nd i ng t ime i s ex tended t he pa r t i c l es become f i ne r , r esu l t i ng
i n t he pos i t i on pa rame te r dec reas ing . Th i s t r end i s p rom inen t
f o r t he gas i f i ca t i on and as we l l as t he b l ended cemen t . The
cemen t c l i n ke r a l one has no c l ea r t r end , s i nce t he pos i t i on
pa rame te r o f t he cemen t a f t e r 30 m inu tes i s l ess t han t ha t o f
i n t e rg r i nd i ng o r gas i f i ca t i on ash . A f t e r 1 hou r t he pos i t i on
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-7
pa rame te rs f o r a l l t h ree a re app rox ima te l y t h e same . He rea f t e r
gas i f i ca t i on ash and i n t e rg r i nd i ng con t i nues t o r educe as
g r i nd i ng t ime i s ex tended , wh i l e t he cemen t i nc reases s l i gh t l y .
01020
30405060
708090
0.5 1 1.5 2 2.5 4
Grinding time (hours)
Posi
tion
Para
met
er X
o (µ
m)
IG
GA
CEM
F igu re 6 .5 Re la t i on be tween g r i nd i ng t ime and pos i t i on
pa rame te r X o
The pos i t i on pa rame te r s o f cemen t r ange be tween 25μm and
38μm an d t he re i s no c l ea r t r end f o r t he pos i t i on pa rame te r o f
cemen t t o r educe w i t h i nc reased g r i nd i ng t ime . The pos i t i on
pa rame te r o f gas i f i ca t i on ash and i n t e rg r i nd i ng i s s i gn i f i can t l y
sma l l e r t han t ha t o f cemen t , even a f t e r 4 hou rs o f g r i nd i ng .
A f t e r 2 hou rs o f g r i nd i ng t he r educ t i on i n pos i t i on pa rame te r f o r
gas i f i ca t i on ash and i n t e rg r i nd i ng i s no t as no t i ceab le as
be fo re . The g raph i nd i ca tes t ha t an exponen t i a l r e l a t i on ex i s t s
be tween pa r t i c l e s i ze and g r i nd i ng t ime . I t seems as i f an
op t imum g r i nd i ng t ime can be es tab l i shed . Fo r bo th the
i n t e rg r i nd i ng and gas i f i ca t i on ash t h i s op t imum seems t o be i n
t he r eg ion o f 2 hou rs . G r i nd ing f o r l onge r t han t h i s op t imum
t ime wou ld no t dec rease t he pa r t i c l e s i ze cons ide rab l y mo re
and wou ld on l y add t o t he cos t o f g r i nd i ng .
I n F i gu re 6 .6 t he s l ope i s p l o t t ed as a f unc t i on o f t he g r i nd i ng
t ime . F rom th i s g raph i t can be seen t ha t f o r i n t e rg r i nd i ng and
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-8
gas i f i ca t i on ash t he g r i nd i ng t ime does no t have an i n f l uence
on t he s l ope (n ) va l ue , wh i ch rep resen t s t he range o f t he
pa r t i c l e s i ze d i s t r i bu t i on o f t he pa r t i c l e s i zes g rea te r t han t he
pos i t i on pa rame te r . I t i s obse rved t ha t f o r t he gas i f i ca t i on ash
and i n t e rg r i nd i ng , t he s l ope a f t e r 2 hou rs g r i nd i ng i s a
max i mum and t he rea f t e r t he s l ope dec reases . Thus a f t e r 2
hou rs t he s i ze r ange i s na r row and any i nc rease o r dec rease i n
g r i nd i ng t ime make t he s i ze r ange w ide r . Fo r cemen t t he r ange
va r i es f o r each g r i nd i ng t ime i n t e r va l . I n t e rg r i nd i ng had t he
l a rge r s l ope (n ) and wou ld have a na r rowe r d i s t r i bu t i on t han
t he gas i f i ca t i on ash and t he cemen t . Th i s d i f f e rence i n s l ope i s
howeve r ve r y sma l l and obse rved t r ends a re no t deemed t o be
s i gn i f i can t .
0
0.2
0.4
0.6
0.8
1
1.2
0.5 1 1.5 2 2.5 4
Grinding time (hours)
Slop
e (n
)
IG
GA
CEM
F igu re 6 .6 Re la t i onsh ip be tween g r i nd i ng t ime and s l ope
pa rame te r (n )
The va lues o f t he ove rs i ze pa r t i c l e s i ze d i s t r i bu t i on pa rame te r s
(D50 ) an d (D10 ) can be seen i n Tab le 6 .3 . These pa rame te r s
can be compa red f o r d i f f e ren t samp les .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-9
Tab le 6 .3 Ove rs i ze pa r t i c l e s i ze d i s t r i bu t i on pa rame te r s
Oversize particle size distribution parameters Sample
D50 (µm) D10 (µm)
3 - 30µm (%) <3 µm (%)
IG,30 min 32.1 113.6 41.73 9.18
IG,1hr 19.4 64.2 55.20 13.76
IG, 1.5hr 14.0 44.4 62.05 18.01
IG, 2hr 13.9 45.4 62.18 18.48
IG, 2.5hr 12.7 43.1 62.74 19.65
IG, 4hr 11.6 37.3 64.44 22.07
GA,30 min 50.9 183.5 31.78 7.34
GA, 1hr 21.2 78.7 48.51 14.82
GA, 1.5hr 15.8 58.9 56.30 16.55
GA, 2hr 12.4 44.1 59.57 22.01
GA, 2.5hr 10.5 40.4 59.79 25
GA, 4hr 7.3 31.3 58.34 32.48
Cem,30 min 26.2 92.8 52.82 5.66
Cem, 1hr 22.2 100.9 57.08 6.32
Cem, 1.5hr 23.9 86.5 55.41 6.83
Cem, 2hr 21.4 83.4 57.94 7.13
Cem, 2.5hr 22.1 85.1 56.99 7.42
Cem, 4hr 22.7 106.7 53.25 7.97
The D50 and D10 resu l t s i n t he t ab l e i nd i ca te t ha t f o r
i n t e rg r i nd i ng o f 35% gas i f i ca t i on ash and 65% cemen t i n t he
ba l l m i l and f o r sepa ra te l y g rou nded gas i f i ca t i on ash and
cemen t t he ove rs i ze pa r t i c l e s i ze d i s t r i bu t i on pa rame t e r s , D50
and D10 , dec rease f o r i nc reased g r i nd i ng t ime . Th i s t r end i s
mo re obse rvab le f o r t he gas i f i ca t i on ash . The gas i f i ca t i on ash
has a so f t e r c l i n ke r t han t h e cemen t and t h i s i s seen s i nce t he
gas i f i ca t i on ash i s eas ie r t o g r i nd . Fo r t he cemen t t he re i s no
c l ea r t r end . Th i s i s due t o t he ha rde r cemen t c l i n ke r . I t seems
t ha t i n c reased g r i nd i ng d i d no t a f f ec t t he pa r t i c l e s i ze . The
t ab le a l so i nd i ca te t he 30 -3µm and <3µm pe rcen tage pa r t i c l es .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-10
These resu l t s i nd i ca te t ha t w i t h i nc reased g r i nd i ng t ime t he %
o f pa r t i c l es <3µm i nc rease . The cemen t r ema ine d a lmos t
cons tan t be tween 52 and 58µm. Fo r bo th t he i n t e rg r i nd ing and
gas i f i ca t i on ash t he % pa r t i c l es become more as g r i nd i ng t ime
i nc rease . A l l o f t he r esu l t s i n t he t ab l e i nd i ca te t ha t w i t h
i nc reased g r i nd i ng t ime t he pa r t i c l es become sma l l e r .
6 .2 .2 Shape o f Par t i c les
Pa r t i c l e shape has a s t r ong i n f l uence on t he wa te r r equ i r emen t
o f conc re te . The un ique sphe r i ca l shape o f f l y ash makes i t s
wa te r r equ i r emen t l owe r and t hus imp roves t he wo rkab i l i t y ( see
F igu re 6 .7 ) . The gas i f i ca t i on ash has no un ique s t r uc tu re and
cou ld be desc r i bed as angu la r as can be seen i n F i gu re 6 .8 .
Angu la r shapes have h i g he r wa te r r equ i r emen ts , and an
i nc rease i n po ros i t y and a dec rease i n s t r eng th may be
expec ted .
F i gu re 6 .7 Scann ing e l ec t ron m i c roscope pho to o f f l y ash
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-11
F igu re 6 .8 Scann ing e l ec t ron m i c roscope pho to o f gas i f i ca t i on
ash
The B la i ne su r f ace a rea (Append i x D ) f o r cemen t , gas i f i ca t i on
ash and i n t e rg round cemen t and gas i f i ca t i on ash i s seen i n
F i gu re 6 .9 .
0
100
200
300
400
500
600
700
800
30 min 1 hour 1.5 hours 2 hours 2.5 hours 4 hours
Grinding time (hours)
Bla
ine
Surf
ace
Are
a m
2 /g
Cement Gasification ash Intergrinding
F i gu re 6 .9 G raph i nd i ca t i ng B la i ne su r f ace a rea
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-12
F rom the g raph i t can be seen t ha t cemen t has a su r face a rea
rang ing be tween 300m 2 /g and 450m 2 /g . Th i s r ange o f su r f ace
a rea co r responds t o commerc i a l cemen t as r epo r t ed by Bha t t y
e t a l ( 2004 ) . The su r f ace a rea o f cemen t i nc rease f o r t he
g r i nd i ng t ime i n t e r va l s up t o 2 hou rs , a f t e r wh i ch t he su r f ace
a rea rema ins cons tan t f o r 2 . 5 hou rs and s l i gh t l y dec reases f o r
4 hou rs g r i nd i ng . Th i s i nd i ca tes t ha t l onge r g r i nd i ng does no t
keep i nc reas ing t he su r f ace a rea . The re seems t o be an
op t imum su r f ace a rea f o r t he cemen t . I n i t i a l l y a f t e r 30
m inu tes , gas i f i ca t i on ash has t he l owes t su r face a rea wh i l e t he
i n t e rg round samp le i s c l ose t o t he cemen t samp le . F rom 1 hou r
g r i nd i ng , bo th t he gas i f i ca t i on ash and i n t e rg round gas i f i ca t i on
ash and cemen t samp le has a h i ghe r su r f ace a rea than t he
cemen t . The gas i f i ca t i on as h and i n t e rg round gas i f i ca t i on ash
and cemen t i s app rox ima te l y t he same up t o 2 hou rs o f g r i nd i ng ,
The rea f t e r t he gas i f i ca t i on ash ’ s su r f ace a rea i nc rease more
t han t he i n t e rg round . Th i s i nd i ca tes t ha t t he su r f ac e a rea o f
gas i f i ca t i on ash i nc rease , wh i l e t he cemen t r eached an
op t imum su r f ace a rea . A f t e r 2 hou rs , when cemen t r eached an
op t imum su r f ace a rea , t he i n t e rg round gas i f i ca t i on ash and
cemen t samp le i nc reased l ess i n su r face a rea .
6 .3 CHEMICAL PROPERTIES
6 .3 .1 XRF
The XRF resu l t s o f t he gas i f i ca t i on ash p rov i ded i ns i gh t i n t o
t he behav iou r i n r eac t i v i t y i n conc re te . The chem ica l
compos i t i on o f bo th gas i f i ca t i on and f l y ash can be seen i n
Tab le 6 .4 .
These resu l t s i nd i ca te t ha t gas i f i ca t i on ash has a chem ica l
compos i t i on s im i l a r t o t ha t o f f l y as h and i t shou ld thus be
accep tab le t o use as a cemen t ex tende r i n conc re te . The re a re
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-13
th ree e l emen ts i n t he f o rm o f ox i des p resen t i n t he gas i f i ca t i on
ash (MnO, C r 2 O 3 and V 2 O 5 ) wh i ch a re no t i n f l y ash . These
e l emen ts shou ld have no e f f ec t on t he r eac t i v i t y . T he P 2 O 5 -
con ten t i s l owe r i n t he gas i f i ca t i on ash bu t was no t cons ide red
t o be s i gn i f i can t . The va ry i ng amoun t o f A l 2 O 3 w i t h i n t he ashes
i s no t so impo r t an t i n de te rm in i ng t he i n f l uence on p rope r t i es
i n conc re te , t hus the l owe r con ten t o f A l 2 O 3 i n gas i f i ca t i on ash
wou ld no t have d e t r imen ta l e f f ec t s on t he conc re te . These
resu l t s i nd i ca te t ha t gas i f i ca t i on ash shou ld be accep tab le t o
use as a cemen t ex tende r i n conc re te .
Tab le 6 .4 XRF resu l t s
E lements Gas i f i ca t ion Ash
%
T yp ica l v a lues o f South A f r i can F l y
Ash* %
Fe 2 O 3 6 .8 3 .7 -4 .7
MnO 0 .13 0
C r 2 O 3 0 .63 0
V 2 O 5 0 .02 0
T iO 2 1 .43 1 .4 -1 .9
CaO 8 .17 7 .1 -10 .5
K 2 O 0 .83 0 .5 -1 .2
P 2 O 5 0 .7 1 .1 -1 .4
S iO 2 48 .5 45 -49
A l 2 O 3 23 .5 29 -31
MgO 2 .3 1 .8 -2 .8
Na 2 O 0 .5 0 .1 -0 .8
C l 0 0
S 0 .4 0
SO 3 0 .49 0 .5 -1 .0
Loss on i gn i t i on 5 .18 5 .0
* (SANS 1491 -2 :2005 / SABS 1491 -2 :2005 )
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-14
6 .3 .2 XRD
The XR D resu l t s showed t ha t gas i f i ca t i on ash has h i gh
pe rcen tages o f qua r t z (S iO 2 ) and mu l l i t e (A l 6 S iO 1 3 ) wh i ch i s
s im i l a r t o f l y ash .
The XRD ana l ys i s o f gas i f i ca t i on as h shows t ha t ano r t h i t e ,
sod ian i n t e rmed ia te ( (Ca , Na ) (S i , A l ) 4 O 8 ) , mu l l i t e (A l 6 S iO 1 3 ) ,
a l pha -qua r t z (S iO 2 ) , we re f ound t o be t he ma jo r m ine ra l s
p resen t i n ash , d i ops i de (Ca (Mg ,A l ) (S i ,A l ) 2 O 6 ) , i nd i a l i t e
(Mg 2 A l 4 S i 5 O 1 8 ) and geh len i t e (Ca 2 A l 2 S iO 7 ) we re i den t i f i ed i n
sma l l concen t ra t i ons . These resu l t s i nd i ca te t ha t gas i f i ca t i on
ash shou ld be accep tab le f o r use as a cemen t ex tende r i n
conc re te .
GASIFICATION
00-015-0776 (I) - Mullite, syn - Al6Si2O13 - Orthorhombic - 00-018-1202 (I) - Anorthite, sodian, intermediate - (Ca,Na)(Si,Al)4O8 - Triclinic - 00-046-1045 (* ) - Quartz, syn - SiO2 - Hexagonal - I/Ic PDF 3.4 - GASIFICATION - File: HANLI04-5.raw - Type: 2Th/Th locked - Start : 5.000 ° - End: 70.000 ° - Step: 0.040 ° - Step time: 1.5 s - Temp.: 25 °C (Room) - Time Started: 0 s - 2-Theta: 5.000 ° - Theta: 2.500 ° - Chi: 0.00 ° -
Lin
(Cou
nts)
0
100
200
300
400
500
600
700
800
900
1000
1100
1200
1300
1400
1500
2 Theta (Cu K-alpha)
6 10 20 30 40 50 60 70
F i gu re 6 .10 XRD resu l t s f o r gas i f i ca t i on ash
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-15
6 .3 .3 S tandard Tes ts fo r Cement i t ious Mate r ia ls
The resu l t s o f t he s t anda rd t es t s conduc ted a re summa r i zed i n
Tab le 6 .5 . The chem ica l requ i r emen ts o f t he gas i f i ca t i on ash
comp ly w i t h t he spec i f i ca t i on as se t f o r f l y ash i n a l l bu t two
cases . The gas i f i ca t i on ash has a h i ghe r l oss on i gn i t i on
( LO I ) , due t o t he h i ghe r ca rbon con ten t , wh i ch g i ves the ash a
da rk g rey co l ou r . The wa te r r equ i r emen t o f gas i f i ca t i on ash i s
mo re t han 100% and t h i s can be exp la i ned when cons ide r i ng
t he angu la r shape o f t he gas i f i ca t i on ash . The s t r eng th f ac to r
o f gas i f i ca t i on ash i s 2% h ighe r t han f l y ash . The f ac to r s t ha t
do no t mee t t he l im i t s as se t f o r f l y ash do no t cause a g rea t
conce rn bu t i t shou ld be i nves t i ga ted .
Tab le 6 .5 Chem ica l t es t r esu l t s
Tes t Me thod Gas i f i ca t ion
ash L imi ts fo r
F l y ash
Su lphu r t r i o x i de con ten t , %
(m /m) SANS 50 196 -2 0 .49 <2 .5
Loss on i gn i t i on , % (m /m) SANS 50 196 -3 5 .18 <5 .0
F ree wa te r con ten t , %
(m /m) SANS 61 51 0 .19 1
F i neness , r es i due re ta i ned
on a s i eve w i t h squa re
ape r t u res o f nom ina l s i ze
45um, % (m /m)
SANS 61 57 6 .5 12 .5
Wa te r r equ i r emen t , % o f
con t ro l , max SANS 61 56 > 100 95
S t reng th f ac to r , % SANS 50 196 -1 8 >6
Soundness , expans ion ,
mm, ma x SANS 50 196 -3 0 <1
Re la t i ve dens i t y LSA Me th od 2 .59 2 .3
Spec i f i c su r f ace a rea ,
c m 2 /g LSA Me th od 7802
No t
quan t i f i ed
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-16
6 .4 EFFECT OF GRI N DING T I ME ON T HE PROPERTIES OF INTERBL ENDE D GASIF ICA T ION A S H AND C EME NT
6 .4 .1 Mor ta r P r ism Co mpress ive S t reng th
F i gu re 6 .11 shows t he r esu l t s f o r i n t e rb l end ing gas i f i ca t i on ash
and cemen t manu fac tu red i n t he l abo ra to r y . See Append i x E f o r
t he mo r t a r p r i sm s t r eng th summary . Bo th t h e gas i f i ca t i on ash
and cemen t c l i nke r we re g round f o r d i f f e ren t t ime i n t e r va l s . A
m i x o f cemen t g r i nded f o r 2 hou rs and no t i n t e rb l ended can
a l so be seen i n t he g raph . F rom the resu l t s i t i s obse rved t ha t
con t i nua l l y , t h roughou t t he s t r eng th deve lopmen t , t he m i x
con ta i n i ng cemen t w i t h 2 hou rs g r i nd i ng t ime had t he h i ghes t
compress i ve s t r eng th . A f t e r 28 days t he 2 .5 hou r m i x was
a lmos t equa l t o t he 2 hou r m i x . The m ix made w i t h cemen t
con ta i n i ng on l y c l i nke r ach ieved t he same compress i ve
s t r eng th a f t e r 28 days . The d i f f e rence i n compress i ve s t r eng th
o f m i xes g r i nded f o r l e ss than 2 hou rs was app rox ima te l y 10
MPa . Th i s d i f f e rence c l ea r l y i nd i ca tes t han g r i nd i ng t ime
shou ld no t be sho r te r t han 2 hou rs .
05
101520253035404550
2 days 7 days 28 days
Days
Com
pres
sive
str
engt
h M
Pa 30 min
1 hour1.5 hours
2 hours
2.5 hours4 hours
Cement (2 hrs)
F i gu re 6 .11 Compress i ve s t r eng ths fo r i n t e rb l end ing
gas i f i ca t i on ash and cemen t f o r d i f f e ren t g r i nd i ng t imes
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-17
The compress i ve s t r eng th r esu l t s o f t he mo r ta r p r i sms a re
de f i ned as a s t r eng th c l ass i n Tab le 6 .6 f r om SANS 50197 -
1 /SABS EN 197 -1 :2000 .
Tab le 6 .6 S t reng th c l asses o f i n t e rb l end ing m i xes g r i nd i ng t ime
30 min 1 hour 1.5
hours 2
hours2.5
hours 4
hours cement (2hrs)
Strength class
N/A to 32.5 N 32.5R 32.5R 42.5 R 42.5 N 42.5 N 42.5 N
Percentage strength
development after 7 days
63% 75% 71% 76% 65% 73% 70%
F rom the s t r eng th c l ass requ i r emen ts t he d i f f e rence i n t he
compress i ve mo r t a r s t r eng th f o r t he m i xes a re h i gh l i gh ted .
G r i nd i ng t imes sho r t e r t han 30 m inu tes does no t ach ieve
s t r eng ths f o r an accep tab le s t r eng th c l ass . Gr i nd i ng t imes o f 1
and 1 .5 hou rs p roduce a cemen t s t r eng th c l ass o f 32 .5R . A
cemen t s t r eng th c l ass o f 42 .5 R was p roduced f o r 2 hou rs
g r i nd i ng t ime and f o r t he g r i nd i ng t imes l onge r t han 2 hou rs
cemen t w i t h a s t r eng th c l ass o f 42 .5 N wa s ach ieved . When
cons ide ra t i on i s g i ven t o t he cemen t g r i nded f o r 2 hou rs and
no t i n t e rb l ended , i t i s c l ea r t ha t gas i f i ca t i on ash had a
con t r i bu t i on t o t he ea r l y s t r eng th deve lopme n t o f t he mo r ta r
p r i sms . Tab le 6 .6 a l so i nd i ca tes t he pe rcen tage o f 28 day
s t r eng th ga ined a f t e r 7 days , wh i ch i nd i ca tes t ha t mo s t l y 70%
o f t he s t reng th i s ach ieved a f t e r 7 days . G r i nd ing f o r 2 hou rs
i nc reased t he 7 day s t r eng th t o 76% o f t he 28 day s t r eng th .
6 .4 .2 Mor ta r P r isms F lexura l S t reng th
The f l exu ra l s t r eng ths o f t he i n t e rb l ended m ixes (F i gu re 6 .12 )
i nd i ca te the same t r end as d i d t he compress i ve s t r eng th f o r t he
m ix g r i n ded f o r 2 hou rs (Append i x E ) . A f t e r 28 days t he
i n t e rb l ended m ixes g r i nded f o r l onge r t han 2 hou rs exceeded
t he f l exu ra l s t r eng th o f t he cemen t on l y m i x . The d i f f e rence i n
f l e xu ra l s t r eng ths f o r t he m i xes was app rox ima te l y 1 MPa ,
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-18
wh i ch i s no t a cons ide rab le d i f f e rence . The f l exu ra l s t r eng th
r esu l t s shows t ha t g r i nd i ng t imes g rea te r t han 2 hou rs ach ieved
be t t e r f l exu ra l s t r eng ths .
0123456789
10
2 days 7 days 28 days
Days
Flex
ural
str
engt
h M
Pa
30 min
1 hour
1.5 hours
2 hours
2.5 hours
4 hours
Cement (2 hrs)
F i gu re 6 .12 F l exu ra l s t r eng ths f o r i n t e rb l end ing gas i f i ca t i on
ash and cemen t f o r d i f f e ren t g r i nd i ng t imes
Tab le 6 .7 g i ves a pe rcen tage o f t he compress i ve s t r eng th
ach ieved by t he f l exu ra l s t r eng th a f t e r 28 days . I t i s expec ted
t ha t t he f l e xu ra l s t r eng th shou ld be 10% o f t he compress i ve
s t r eng th . A l l o f t he m i xes had a f l e xu ra l s t r eng th o f a t l eas t
19% o f t he compress i ve s t r eng th . The resu l t s i nd i ca te t ha t
i n t e rb l end ing gas i f i ca t i on ash and cemen t ach ieved be t t e r
f l e xu ra l s t r eng ths than a cemen t on l y m i x .
Tab le 6 .7 Pe rcen tage o f compress i ve s t r eng th ach ieved f o r
i n t e rb l end ing
30 min 1 hour 1.5 hours
2 hours
2.5 hours
4 hours
cement (2hrs)
Percentage of
compressive strength achieved
24% 22% 21% 19% 19% 20% 18%
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-19
6 .4 .3 Par t i c le S i ze D is t r ibu t ion
The e f f ec t o f t he pa r t i c l e s i ze d i s t r i bu t i on on t h e 28 -day
compress i on s t r eng ths can be seen i n F i gu re 6 .13 and F igu re
6 .14 . The Ros in -Rammle r pa r t i c l e s i ze d i s t r i bu t i on pa rame te r s
( as d i scussed i n 4 .3 .1 .2 ) a re p l o t t ed as a f unc t i on o f t he 28 -
day comp ress ion s t r eng ths .
The g raph i nd i ca tes t ha t t he compress i ve s t r eng th i nc reased
w i t h dec reas ing pos i t i on pa rame te r s ( X o ) f o r i n t e rb l end ing o f
cemen t c l i n ke r and gas i f i ca t i on ash . Thus f i ne r pa r t i c le
ach ieved g rea te r s t r eng ths . The i n t e rb l ended m ix o f 4 hou rs
g r i nd i ng t ime had t he sma l l es t pos i t i on pa rame te r ( X o ) , bu t
ach ieved s l i gh t l y l owe r s t r eng ths t han t he 2 .5 hou r and 2 hou r
m i xes . I t can be seen i n F i gu re 6 .13 t ha t f o r g r i nd i ng t imes
l onge r t han 2 hou rs t he pos i t i on pa rame te r (X o ) dec reases
s l i gh t l y wh i l e no s i gn i f i can t i n c rease i n compress i ve s t r eng th i s
obse rved .
0
10
20
30
40
50
0 10 20 30 40 50
Position parameter X o (μm)
Com
pres
sive
Str
engt
h M
Pa
IB,30 minIB, 1hr
IB, 1.5hr
IB, 2hrIB, 2.5hr
IB, 4hr
F igu re 6 .13 Re la t i on be tween compress i ve s t r eng ths and
Ros in -Rammle r d i s t r i bu t i on pos i t i on pa rame te r ( X o ) f o r
i n t e rb l end ing gas i f i ca t i on ash and cemen t
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-20
F igu re 6 .13 i nd i ca tes t ha t pos i t i on pa rame te r s l a rge r t han
30μm ac h ieved l owe r compress i ve s t r eng ths . The re was a
cons ide rab le i nc rease i n compress i ve s t r eng th f r om 30μm to
25μm. F rom the g raph i t seems as i f a peak i s r eached a t 25μm,
whe re t he h i ghes t s t r eng ths we re r eached . I t i s t hus conc luded
t ha t 25μm, and t hus 2 hou rs i s an op t imum when pos i t i on
pa rame te rs i s compa red t o t he compress i ve s t r eng th . Howeve r ,
t he d i f f e rence i n compress i ve s t r eng th be tween t he 2 , 2 . 5 and
4 hou rs a re sma l l and t hus a 2 -hou r g r i nd i ng t ime seems t he
mos t e f f ec t i ve when cons ide r i ng s t r eng th , pa r t i c l e s i zes and
cos t o f g r i nd i ng .
I n F i gu re 6 .14 t he s l ope (n ) i s p l o t t ed as a f unc t i on o f t he 28 -
day compress ion s t r eng th . The sma l l es t s l ope , a f t e r 4 hou rs
g r i nd i ng had h i gh compress i ve s t r eng th . G r i nd i ng t imes o f 2
and 2 .5 hou rs had app rox ima te l y t he s ame co mpress i ve
s t r eng ths bu t h i ghe r s l opes . The re i s no c l ea r t r end t o
es tab l i sh t ha t sma l l e r s l opes g i ve h i ghe r compress i ve s t r eng ths .
Howeve r , t he d i f f e rence i n compress ion s t r eng th be tween t he 2
and 4 hou r g r i nd i ng t ime i s sma l l and op t ima l l y t h e 2 hou r
g r i nd i ng t ime i s mos t e f f ec t i ve when s t r eng th , pa r t i c l e s i ze and
cos t o f g r i nd i ng i s cons ide red .
0
10
20
30
40
50
0.85 0.9 0.95 1
Slope (n )
Com
pres
sive
str
engt
h (M
Pa)
IB,30 min
IB, 1hr
IB, 1.5hr
IB, 2hr
IB, 2.5hr
IB, 4hr
F igu re 6 .14 Re la t i on be tween compress i on s t r eng ths and
Ros in -Rammle r d i s t r i bu t i on s l ope ( n ) pa rame te r f o r
i n t e rb l end ing gas i f i ca t i on ash and cemen t
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-21
I n F i gu re 6 .15 , t he ove rs i ze pa r t i c l e s i ze d i s t r i bu t i on
pa rame te r s (D50 ) and (D10 ) a re p l o t t ed as a f unc t i on o f t he 28 -
day compress i ve s t r eng th i n o rde r t o f i nd t he i n f l uence o f
compress i ve s t r eng th on t he pa r t i c l es s i ze d i s t r i bu t i on .
25
30
35
40
45
50
0 20 40 60 80 100 120 140
Oversize Particle size distribution parameters (μm)
Com
pres
sive
Str
engt
h (M
Pa)
IB,30 min
IB, 1hr
IB, 1.5hr
IB, 2hr
IB, 2.5hr
IB, 4hr
F igu re 6 .15 Re la t i on be tween compress ion s t r eng th and
pa r t i c l e s i ze d i s t r i bu t i on pa rame te r s f o r i n t e rb l end ing
gas i f i ca t i on ash and cemen t
As t he ave rage pa r t i c l e s i ze becomes sma l l e r t he 28 -day
compress ion s t r eng th i nc reases . As t he 10% l a rges t pa r t i c l e
s i ze f o r d i f f e ren t g r i nd i ng t imes become sma l l e r compress i ve
s t r eng ths a l so i nc reases . A f t e r 2 h ou rs g r i nd i ng t he max i mum
compress i ve s t r eng th i s ob ta i ned . The d i f f e rence i n
compress i ve s t r eng th be tween 2 , 2 . 5 and 4 hou rs i s sma l l and
t hus an op t imum l im i t i s r eac hed a f t e r 2 hou rs g r i nd i ng f o r bo th
t he 50% and 10% l a rges t pa r t i c l e s i ze d i s t r i bu t i on pa rame te r s .
D50 D10
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-22
6 .5 EFFECT OF GRI N DING T I ME ON T HE PROPERTIES OF INTER GR OUN D GASIF ICA T ION A S H AND C EME NT
6 .5 .1 Mor ta r P r ism Co mpress ive S t reng th
F i gu re 6 .16 shows t he r esu l t s f o r gas i f i ca t i on ash and cemen t
c l i n ke r i n t e rg round i n t he b a l l m i l l f o r d i f f e ren t t ime i n t e r va l s .
See summary o f s t r eng th r esu l t s i n Append i x F . The resu l t s
i nd i ca te t ha t i n t e rg r i nd i ng f o r 2 hou rs ach ieved t he h i ghes t
compress i ve s t r eng th du r i ng t he s t reng th deve lopmen t . Same
as f o r t he i n t e rb l end ing , g r i nd i ng f o r sho r te r t han 1 .5 hou rs
ach ieved s t r eng ths o f app rox ima te l y 10 MPa l ess . The
compress i ve s t r eng th o f t he cemen t on l y m i x whe re s l i gh t l y
h i ghe r t han t he m ixes i n t e rg round f o r l onge r t han 2 hou rs . Th i s
d i f f e rence o f 1 MPa i s omiss i b l e . F rom the resu l t s i t can be
seen t ha t i n t e rg r i nd i ng t ime shou ld no t be sho r t e r t han 1 .5
hou rs .
05
101520253035404550
2 days 7 days 28 days
Days
Com
pres
sive
str
engt
h M
Pa 30 min
1 hour
1.5 hours
2 hours
2.5 hours
4 hours
Cement (2 hrs)
F i gu re 6 .16 Compress i ve S t reng th f o r i n t e rg r i nd i ng gas i f i ca t i on
ash and cemen t f o r d i f f e ren t g r i nd i ng t imes
F rom th e s t r eng th c l ass r equ i r emen ts i n Tab le 6 .7 t he
d i f f e rence i n i n t e rb l end ing and i n t e rg r i nd i ng can be obse rved i n
t e rms o f s t r eng th . G r i nd ing t imes sho r t e r t han 30 m i nu tes f o r
i n t e rg r i nd i ng d i d no t ach ieve s t r eng ths f o r an accep tab le
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-23
s t reng th c l ass . The same s t r eng th c l ass we re ach ieved f o r
g r i nd i ng 1 , 1 . 5 , 2 and 4 hou rs . Fo r i n t e rg r i nd i ng t he 2 .5 hou r
g r i nd i ng ach ieved a l owe r s t r eng th c l ass t han w i t h t he
i n t e rb l end ing a t 32 .5 R . T h i s i s s im i l a r t o t he 1 and 1 .5 hou r
g r i nd i ng t ime s t r eng th c l as s . A cemen t s t r eng th c l ass o f 42 .5 R
was p roduced f o r 2 hou rs g r i nd i ng t ime an d f o r g r i nd i ng 4
hou rs cemen t w i t h a s t r eng th c l ass o f 42 .5 N was ach ieved .
When cons ide ra t i on i s g i ven t o t he cemen t g r i nded fo r 2 hou rs
and no t i n t e rb l ended , i t i s c l ea r t ha t gas i f i ca t i on as h had a
con t r i bu t i on t o t he ea r l y s t r eng th deve lopme n t o f t he mo r ta r
p r i sms .
Tab le 6 .8 a l so i nd i ca tes t he pe rcen tage o f 28 day s t r eng th
ga ined a f t e r 7 days , wh i ch i nd i ca tes t ha t a t l eas t 70% o f t he
s t r eng th i s ac h ieved a f t e r 7 days f o r a l l t he m i xes .
I n t e rg r i nd i ng ach ieved a f as te r r a te o f s t r eng th deve lopmen t
a f t e r 7 days t han t he i n t e rb l end ing m ixes (Tab le 6 .6 ) .
Tab le 6 .8 S t reng th c l asses fo r i n t e rg r i nd i ng m i xes g r i nd i ng t ime
30 min 1
hour 1.5
hours 2
hours2.5
hours 4
hours cement (2hrs)
Strength class
N/A to 32.5 N 32.5R 32.5R 42.5 R 32.5 R 42.5 N 42.5 N
Percentage strength
development after 7 days
71% 75% 73% 75% 76% 73% 70%
6 .5 .2 Mor ta r P r ism F lexura l S t reng th
The f l exu ra l s t r eng ths o f i n t e rg r i nd i ng i n F i gu re 6 .17 i nd i ca te
t ha t g r i nd i ng t imes l onge r t han 1 .5 hou rs ach ieved h i ghe r
f l e xu ra l s t r eng ths (Append i x F ) . The d i f f e rence i n f l e xu ra l
s t r eng ths i s l ess than 1 MPa . The g raph i nd i ca tes t ha t a l t hough
t he d i f f e rence i n f l e xu ra l s t r eng t h i s om iss i b l e , g r i nd i ng t imes
l onge r t han 1 .5 hou rs ach ieved g rea te r f l e xu ra l s t r eng ths and
t hus g r i nd i ng f o r l e ss t han 1 .5 hou rs i s no t adv i sab le .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-24
0123456789
10
2 days 7 days 28 days
Days
Flex
ural
str
engt
h M
Pa 30 min
1 hour1.5 hours
2 hours
2.5 hours4 hours
Cement (2 hrs)
F i gu re 6 .17 F lexu ra l s t r eng ths f o r i n te rg r i nd i ng gas i f i ca t i on ash
and cemen t
Tab le 6 .9 g i ves a pe rcen tage o f t he compress i ve s t r eng th
ach ieved by t he f l e xu ra l s t r eng th a f t e r 28 days f o r i n t e rg r i nd i ng .
A l l o f t he m i xes had a f l e xu ra l s t r eng th o f a t l eas t 20% o f t he
compress i ve s t r eng th , wh i ch i s h i ghe r t han t he expec ted 10%.
The l owes t pe rcen tage i s ac h ieved by t he cemen t on l y m i x . The
resu l t s i nd i ca te t ha t i n t e rg r i nd i ng gas i f i ca t i on ash and cemen t
ach ieved be t t e r f l exu ra l s t r eng ths t han a cemen t on l y m i x .
Tab le 6 .9 Pe rcen tage o f compress i ve s t r eng th ach ieved f o r
i n t e rg r i nd i ng
30 min 1
hour 1.5
hours 2
hours2.5
hours 4
hours cement (2hrs)
Percentage of
compressive strength achieved
26% 24% 22% 20% 22% 20% 18%
6 .5 .3 Par t i c le S i ze D is t r ibu t ion
The e f f ec t o f t he pa r t i c l e s i ze d i s t r i bu t i on on t h e 28 -day
compress i on s t r eng ths can be seen i n F i gu re 6 .18 and F igu re
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-25
6 .19 . The Ros in -Rammle r pa r t i c l e s i ze d i s t r i bu t i on pa rame te r s
( as d i scussed i n 4 .3 .1 .2 ) a re p l o t t ed as a f unc t i on o f t he 28 -
day comp ress ion s t r eng ths .
The g raph i nd i ca tes t ha t compress i ve s t r eng th i nc rease w i th
dec reas ing pos i t i on pa rame te r s (X o ) f o r i n t e rg r i nd i ng o f cemen t
c l i n ke r and gas i f i ca t i on ash . Thus f i ne r pa r t i c l e ach ieved
g rea te r s t r eng ths . I t can be seen i n F i gu re 6 .18 t ha t f o r
g r i nd i ng t imes l onge r t han 2 hou rs the pos i t i on pa rame te r (X o )
dec reases s l i gh t l y wh i l e no s i gn i f i can t i n c rease i n compress i ve
s t r eng th i s obse rved .
0
10
20
30
40
50
0 10 20 30 40 50 60
Position parameter X o (μm)
Com
pres
sive
Str
engt
h M
Pa
IG,30 min
IG,1hr
IG, 1.5hrIG, 2hr
IG, 2.5hr
IG, 4hr
F i gu re 6 .18 Re la t i on compress i ve s t r eng ths and Ros in -Rammle r
d i s t r i bu t i on pos i t i on pa rame te r ( X o ) f o r i n t e rg r i nd ing
gas i f i ca t i on ash and cemen t
F i gu re 6 .19 i nd i ca tes t ha t pos i t i on pa rame te r s l a rge r t han
20μm ac h ieved cons ide rab l y l owe r compress i ve s t r eng ths .
The re was a cons ide rab le i nc rease i n compress i ve s t r eng th
f r om 30μm to 20μm. The h i ghes t s t r eng ths we re r eached a t
20μm an d 16μm. The 30 -3µm used by cemen t manu fac tu re r s as
a l im i t on f i neness , e f f ec t i ve l y show tha t a f t e r 1 .5 hou rs t he %
pa r t i c l e a lmos t r ema ined cons tan t (Tab le 6 .3 ) as d i d t he
compress i ve s t r eng th . F rom the g raph i t seems as i f a peak i s
r eached a t 20μm. I t i s t hus conc luded t ha t 20μm, an d t hus 2
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-26
hou rs i s an op t imum when pos i t i on pa rame te r s i s compa red t o
t he compress i ve s t r eng th .
0
10
20
30
40
50
0.97 0.975 0.98 0.985 0.99 0.995 1
Slope (n )
Com
pres
sive
str
engt
h (M
Pa)
IG,30 min
IG,1hrIG, 1.5hr
IG, 2hr
IG, 2.5hrIG, 4hr
F i gu re 6 .19 Re la t i on be tween 28 -day compre ss ion s t reng ths
and Ros in -Ramml e r d i s t r i bu t i on s l ope ( n ) pa rame te r
I n F i gu re 6 .19 t he s l ope (n ) i s p l o t t ed as a f unc t i on o f t he 28 -
day compress ion s t r eng th . F rom th i s g raph i t seems t ha t w i t h
i nc reased g r i nd i ng t ime t he s l ope (n ) dec rease and t he
compress i on s t r eng ths i nc rease . The sma l l es t s l ope , a f t e r 4
hou rs g r i nd i ng had t he g rea tes t compress i on s t r eng th . Aga in
t he d i f f e rence i n compress ion s t r eng th be tween t he 2 and 4
hou r g r i nd i ng t ime i s sma l l and op t ima l l y t he 2 hou r g r i nd i ng
t ime i s mos t e f f ec t i ve when s t r eng th , pa r t i c l e s i ze and cos t o f
g r i nd i ng i s cons ide red .
I n F i gu re 6 .20 , t he ove rs i ze pa r t i c l e s i ze d i s t r i bu t i on
pa rame te r s (D50 ) and (D10 ) a re p l o t t ed as a f unc t i on o f t he 28 -
day compress i ve s t r eng th i n o rde r t o f i nd t he i n f l uence o f
compress i ve s t r eng th on t he pa r t i c l es s i ze d i s t r i bu t i on .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-27
25
30
35
40
45
50
0 20 40 60 80 100 120
Oversize Particle size distribution parameters (μm)
28-D
ay C
ompr
essi
ve S
tren
gth
(MPa
)
IG,30 min
IG,1hr
IG, 1.5hr
IG, 2hr
IG, 2.5hr
IG, 4hr
F i gu re 6 .20 Re la t i on be tween 28 -day compress ion s t reng th and
pa r t i c l e s i ze d i s t r i bu t i on pa rame te r s
D50 D10
As t he ave rage pa r t i c l e s i ze becomes sma l l e r t he 28 -day
compress ion s t r eng th i nc reases . As t he 10% l a rges t pa r t i c l e
s i ze f o r d i f f e ren t g r i nd i ng t imes become sma l l e r compress i ve
s t r eng ths a l so i nc reases . I t i s i n te res t i ng t o no te tha t t he
d i s t r i bu t i on cu r ves conve rge , i nd i ca t i ng t ha t t he pa r t i c l e s i zes
become sma l l e r and more u n i f o rm i n s i ze a t h i ghe r s t r eng ths .
A f t e r 4 h ou rs g r i nd i ng t he ma x imu m compress i ve s t r eng th i s
ob ta i ned . Howeve r t he compress i ve s t r eng th d i f f e rence
be tween 4 hou rs and 2 hou rs i s sma l l and t hus an op t imum
l im i t i s r eached a f t e r 2 ho u rs g r i nd i ng f o r bo th t he 50% and
10% l a rges t pa r t i c l e s i ze d i s t r i bu t i on pa rame te r s .
6 .6 EFFECT OF GYPSUM CONTENT ON THE PROPERTIES OF INTER GR OUN D GASIF ICA T ION A S H AND C EME NT
6 .6 .1 Mor ta r P r ism Co mpress ive S t reng th
F igu re 6 .21 shows t he compress i ve r esu l t s f o r d i f f e ren t gypsum
con ten t s . See App end i x G f o r a summary o f t he s t r eng ths . The
h i ghes t compress i ve s t r eng th i s ach ieved by 3% gypsum
con ten t bu t t he d i f f e rence i n compress i ve s t r eng th f o r t he
d i f f e ren t gypsum con ten t s i s no t s i gn i f i can t . A l l o f t he m i xes
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-28
can be c l ass i f i ed as 32 .5R i n s t r eng th c l ass . F rom th e resu l t s
t he re i s no c l ea r i nd i ca t i on t ha t t he re i s an op t imum gypsum
con ten t .
0
5
10
15
20
25
30
35
40
45
2 Days 7 Days 28 Days
Days
Com
pres
sive
Str
engt
h M
Pa
0%
0.50%
1%
1.50%
2%
2.50%
3%
F igu re 6 .21 Compress i ve s t r eng ths fo r gypsum con ten t
6 .6 .2 Mor ta r P r ism F lexura l S t reng th
The f l exu ra l s t r eng ths (Append i x G ) f o r d i f f e ren t gypsum
con ten t s can be seen i n F i gu re 6 .22 . A l l o f t he m i xe s we re a
b l end o f 35% gas i f i ca t i on ash , i n t e rg r i nded w i t h cemen t . A f t e r
28 days t he h i ghes t compress i ve s t r eng th i s ach ieved by 2%
gypsum c on ten t . The d i f f e rence i n compress i ve s t r eng th f o r t he
d i f f e ren t m i xes i s sma l l . F rom the f l e xu ra l s t r eng th r esu l t s
t he re i s no c l ea r i nd i ca t i on t ha t t he re i s an op t imum gypsum
con ten t .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-29
012345
6789
10
2 Days 7 Days 28 Days
Days
Flex
ural
Str
engt
h M
Pa 0%
0.50%
1%
1.50%
2%
2.50%3%
F igu re 6 .22 F lexu ra l s t r eng ths f o r gypsum con ten t
6 .6 .3 Hea t o f Hyd ra t io n
F igu re 6 .23 shows t he ra te o f hea t deve lopmen t f o r d i f f e ren t
gypsum pe rcen tages . F rom the g raph i t i s obse rved t ha t t he
f i r s t peak ( i n i t i a l r eac t i on ) i s de layed f o r l ow pe rcen tages o f
gypsum. A l l t he f i r s t peaks f o r t he gypsum pe rcen tages have a
l owe r hea t evo lu t i on t han t he re fe rence 100% cemen t m i x . A
3% rep lacemen t o f gypsum peaks a t t he same t ime as t he 100%
cemen t , howeve r a t a l ower hea t evo lu t i on . Fo r a l l t he cu r ves i t
i s obse rved t ha t t he cu r ves a re smoo th and no shou lde rs i s
obse rved a f t e r t he f i r s t hea t peak wh i ch wou ld i nd i ca te f l a sh o r
f a l se se t . The du ra t i on f o r t es t i ng was 36 hou rs and res t r i c t s
t he comp le te cu r ve o f hyd ra t i on .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-30
0
0.5
1
1.5
2
2.5
0.02 3 6 8 11 14 17 19 22 25 28 30 33 36
Time (hrs)
dQ/d
t (m
wat
ts/g
.sec
)
1 cem 0% gypsum 1 cem 0.5% gypsum 1 cem 1% gypsum 1 cem 1.5% gypsum1 cem 2% gypsum 1 cem 2.5% gypsum 1 cem 3% gypsum Cement 100%
F igu re 6 .23 Ra te o f hea t deve lopmen t f o r d i f f e ren t gypsum
pe rcen tages
F i gu re 6 .24 rep resen t s t he evo lu t i on o f t he hyd ra t i on hea t o f
mo r ta r s made w i t h t he d i f f e ren t pe r cen t o f gypsum su bs t i t u t i on
r e l a t i ve t o 100% PC mor t a r , w i t h a r e fe rence po in t o f ze ro
be ing ass i gned t o t he hyd ra t i on hea t deve loped by t h e 100%
PC mor ta r . Th i s r ep resen ta t i on o f t he da ta shows c l ea r l y t he
e f f ec t o f d i f f e ren t pe r cen tages o f gypsum on t he hea t
deve lopmen t . Low pe rcen tages o f gypsum dec rease t he hea t
ou tpu t a f t e r t he i nduc t i on pe r i od . The hea t d i f f e rence w i th
r espec t t o t he pu re cemen t pas te i s pos i t i ve f o r t hes e m ixes
a f t e r t he i nduc t i on pe r i od . Fo r h i ghe r gypsum pe rcen tages t he
i n i t i a l hea t ou tpu t i s l e ss t han f o r l ow gypsum pe rcen tages .
A f t e r t he i nduc t i on pe r i od t he hea t d i f f e rence f o r t he h i ghe r
gypsum pe rcen tages as nega t i ve . H ighe r gypsum p e rcen tages
seem to have a cons tan t hea t ou tpu t a f t e r t he i nduc t i on pe r i od .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-31
-1.8
0
1.80.
02 2 4 6 8 10 12 14 16 18 20 22 24 26 28 30 32 34 36
Time (hours)
Δ (d
Q/d
t)
1 cem 0% gypsum 1 cem 0.5% gypsum 1 cem 1% gypsum1 cem 1.5% gypsum 1 cem 2% gypsum 1 cem 2.5% gypsum1 cem 3% gypsum
F igu re 6 .24 The d i f f e rence i n t he r a te o f hea t evo lu t i on f o r
d i f f e ren t gypsum p e rcen tages cemen t and pu re PC cemen t
Th i s was f u r t he r con f i rmed by t he p l o t t i ng t he t o ta l hea t
evo l ved w i t h t ime i n F i gu re 6 .25 . The t o ta l hea t evo l ved a t t h e
f i r s t 10 hou rs i nc reased w i t h dec reas ing gypsum con ten t s .
A f t e r 10 hou rs t he pu re cemen t has a cons ide rab le i nc rease i n
hea t whe re l ow gypsum pe rcen tages dec rease the hea t
evo lu t i on . H ighe r gypsum pe rcen tages have a cons tan t hea t
evo lu t i on wh i ch i s l owe r t han t he pu re cemen t . F rom the resu l t s
i t i s c l ea r l y obse rved t ha t gypsum d ec rease the hea t evo lu t i on
o f cemen t pas tes . Th i s i s t r ue f o r t he sma l l es t pe r cen tages o f
gypsum. The re i s no c l ea r i nd i ca t i on t ha t gypsum pe rcen tages
cons ide rab l y enha nce t he hyd ra t i on o f cemen t . I t can be
deduced t ha t a 2 .5% gypsum add i t i on i s a good ave ra ge t o use
i n f u r t he r t es t i ng when hea t o f hyd ra t i on and compress i ve
s t r eng th i s cons ide red .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-32
0
40
80
120
160
200
240
0 10 20 30 40
Time (hours)
Q (m
Wat
ss/g
)
Cum 0%
Cum 0.5%
Cum 1%
Cum 1.5%
Cum 2%
Cum 2.5%
Cum 3%
Cum cement
F igu re 6 .25 To ta l hea t o f hyd ra t i on o f d i f f e ren t gypsum
pe rcen tage cemen ts a t 25 ºC
6 . 7 EFFECT OF REPL ACE MENT LEVEL ON THE PROPERTIES OF
INTER GR OUN D GASIF ICA T ION A S H AND C EME NT 6 .7 .1 Mor ta r P r ism Co mpress ive S t reng th
F i gu re 6 .26 shows t he r esu l t s f o r gas i f i ca t i on ash and cemen t
c l i n ke r i n t e rg round f o r d i f f e ren t r ep lacemen t l eve l s . See
Append i x H f o r summary o f s t r eng th r esu l t s . The resu l t s
i nd i ca te tha t a r ep lacemen t l eve l o f 10% ach ieved t he h i ghes t
compress i ve s t r eng th . Rep lacemen t l eve l s mo re t han 10% we re
g radua l l y l owe r i n compress i ve s t r eng th . Rep lac i ng 10% o f
cemen t w i t h gas i f i ca t i on ash ach ieved a h i ghe r compress i ve
s t r eng th t han t he m i x w i t h 0% rep lacemen t . T h i s c l ea r l y
i nd i ca tes t ha t gas i f i ca t i on ash rep l acemen t can i nc rease t he
compress i ve s t r eng th o f mo r ta r pas tes . The d i f f e rence i n
compress i ve s t r eng th be tween 35% and 55% i s app rox ima te l y
15MPa , wh i ch i s cons ide rab le . F rom the resu l t s i t can be seen
t ha t a 10% rep lacemen t o f gas i f i ca t i on ash had t he h i ghes t
compress i ve s t r eng th . The 20% and 35% rep lacemen t ha d
l owe r compress i ve s t r eng ths bu t was s t i l l cons ide red as
su f f i c i en t f o r use i n cemen t . A r ep l acemen t o f 55% had l ow
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-33
compress i ve s t r eng ths and i s no t r ecommende d as a
r ep lacemen t f o r cemen t .
010203040506070
2 Days 7 Days 28 Days
Days
Com
pres
sive
Str
engt
h M
Pa0%
10%
20%
35%
55%
F igu re 6 .26 Compress i ve s t r eng th f o r d i f f e ren t r ep lacemen t
l eve l s o f gas i f i ca t i on ash
F rom th e s t r eng th c l ass r equ i r emen ts i n Tab le 6 .10 t he
d i f f e rence i n r ep lacemen t l eve l can be obse rved i n t e rms o f
s t r eng th . Rep lacemen t l eve l s o f 0% to 20% ach ieved t he same
s t r eng th c l ass , 52 .5N . The 35% rep lacemen t ach ieved
s t r eng ths f o r a l owe r s t r eng th c l as s , 42 .5N . The 55% d id no t
ach ieve a compress i ve s t reng th t o be c l ass i f i ed . The resu l t s
i nd i ca te t ha t gas i f i ca t i on ash rep lac emen t has no de t r imen ta l
e f f ec t on t he compress i ve s t r eng th deve lopmen t o f cemen t
pas te . Low rep lacemen t l eve l s ach ieved h i ghe r compress i ve
s t r eng ths t han h i gh rep lacemen t l eve l s .
Tab le 6 .10 a l so i nd i ca tes t he pe rcen tage o f 28 day s t r eng th
ga ined a f t e r 7 days , wh i ch i nd i ca tes t ha t a t l eas t 75% o f t he
s t r eng th i s ach ieved a f t e r 7 days f o r m i xes w i t h a r ep lacemen t
l eve l be tween 0% and 35%. The 10% and 20% rep lacemen t
l eve l ach ieved a fas te r r a te o f s t r eng th deve lopmen t a f t e r 7
days t han t he 0% rep lacemen t l eve l . The 55% rep lacemen t
l eve l ach ieved l owe r s t r eng th deve lopmen t t han t he expec ted
70%.
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-34
Tab le 6 .10 S t reng th c l asses f o r d i f f e ren t r ep lacemen t l eve l s o f
gas i f i ca t i on ash
0% 10% 20% 35% 55%
Strength class 52.5 N 52.5 N 52.5 N 42.5 N N/A to 32.5N
Percentage strength
development after 7 days
83% 87% 85% 75% 58%
6 .7 .2 Mor ta r P r ism F lexura l S t reng th
The f l exu ra l s t r eng ths (Append i x H ) o f d i f f e ren t r ep lacemen t
l eve l s o f gas i f i ca t i on ash i n F i gu re 6 .27 i nd i ca te t ha t
r ep lacemen t l eve l s l owe r t han 35% ach ieved h i ghe r f l e xu ra l
s t r eng ths . The d i f f e rence i n f l e xu ra l s t r eng ths i s app rox ima te l y
1 MPa . The g raph i nd i ca tes t ha t a l t hough t he d i f f e rence i n
f l e xu ra l s t r eng th i s sma l l , r ep l acemen t l eve l s l ess t han 35%
ach ieved g rea te r f l e xu ra l s t r eng ths and t hus a 55%
rep lacemen t l eve l i s no t adv i sab le .
0.02.04.06.08.0
10.012.0
Tension 2 Days 7 Days
Days
Flex
ural
Str
engt
h M
Pa
0%
10%20%
35%
55%
F igu re 6 .27 F lexu ra l s t r eng ths f o r d i f f e ren t r ep lacemen t l eve l s
o f gas i f i ca t i on ash
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-35
Tab le 6 .11 g i ves a pe rcen tage o f t he compress i ve s t r eng th
ach ieved by t he f l e xu ra l s t r eng th a f t e r 28 days f o r i n t e rg r i nd i ng .
A l l o f t he m i xes had a f l e xu ra l s t r eng th o f a t l eas t 20% o f t he
compress i ve s t r eng th , wh i ch i s h i ghe r t han t he expec ted 10%.
The cemen t on l y m i x seen i n Tab le 6 .7 and 6 .9 had a
pe rcen tage o f 18% wh i l e t he 0% rep lacemen t was 17%. The
ra t i o va r i ed w i t h r epea t i ng and f u r t he r t es t i ng shou ld be done
t o es tab l i sh l im i t s on t he s t r eng ths . The l owes t pe rcen tage i s
ach ieved by t he cemen t on l y m i x . The resu l t s i nd i ca te t ha t
i n t e rg r i nd i ng gas i f i ca t i on ash and cemen t ach ieved be t t e r
f l e xu ra l s t r eng ths than a cemen t on l y m i x .
Tab le 6 .11 Pe rcen tage o f compress i ve s t r eng th ach ieved f o r
d i f f e ren t r ep l acemen t l eve l s o f gas i f i ca t i on ash
0% 10% 20% 35% 55%
Percentage of compressive
strength achieved
17% 17% 18% 22% 26%
6 .7 .3 Par t i c le S i ze D is t r ibu t ion
The e f f ec t o f t he pa r t i c l e s i ze d i s t r i bu t i on on t h e 28 -day
compress i on s t r eng ths can be seen i n F i gu re 6 .28 and F igu re
6 .29 . The Ros in -Rammle r pa r t i c l e s i ze d i s t r i bu t i on pa rame te r s
( as d i scussed i n 4 .3 .1 .2 ) a re p l o t t ed as a f unc t i on o f t he 28 -
day comp ress ion s t r eng ths .
The g raph i nd i ca tes t ha t compress i ve s t r eng th dec rease w i t h
dec reas ing pos i t i on pa rame te r s (X o ) f o r r ep lacemen t l eve l s o f
gas i f i ca t i on ash . I t can be seen i n F i gu re 6 .28 t ha t f o r a 10%
rep lacemen t l eve l o f gas i f i ca t i on as h t he pos i t i on pa rame te r
(X o ) i s sma l l e r t han t he 0% rep lacemen t . Rep lacemen t l eve l s o f
20% and 55% had t he same pos i t i on pa rame te r (Xo ) as t he 10%
rep lacemen t l eve l , bu t w i t h l owe r compress i ve s t r eng ths . The
35% rep lacemen t l eve l had a sma l l e r pos i t i on pa rame te r ( Xo )
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-36
than t he o the r r ep l acemen t l eve l s . The re i s no i nd i ca t i on t ha t
f i ne r pa r t i c l e ach ieved g rea te r s t r eng ths .
010203040506070
0 10 20 30 40
Position parameter X o (μm)
Com
pres
sive
Str
engt
h M
Pa0%
10%
20%
35%
55%
F igu re 6 .28 Re la t i on compress i ve s t r eng ths and Ros in -Rammle r
d i s t r i bu t i on pos i t i on pa rame te r (X o ) f o r r ep lacemen t l eve l s o f
gas i f i ca t i on ash
F i gu re 6 .28 i nd i ca tes t ha t t he re i s no s i gn i f i can t i nd i ca t i on t ha t
pos i t i on pa rame te r s had an e f f ec t on t he compress i ve s t r eng th
deve lopmen t o f t he mo r ta r m i xes .
010203040506070
0.1 0.3 0.5 0.7 0.9 1.1
Slope n
Com
pres
sive
Str
engt
h M
Pa
0%
10%
20%
35%
55%
F igu re 6 .29 Re la t i on be tween 28 -day compre ss ion s t reng ths
and Ros in -Ramml e r d i s t r i bu t i on s l ope ( n ) pa rame te r
I n F i gu re 6 .29 t he s l ope (n ) i s p l o t t ed as a f unc t i on o f t he 28 -
day compress ion s t r eng th . F rom th i s g raph i t seems t ha t t he
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-37
s lope (n ) i s app rox ima te l y 1 f o r a l l t he r ep lac emen t l eve l s o f
gas i f i ca t i on ash bu t 0%. T he compress i ve s t r eng th dec reased
f o r d i f f e ren t r ep lac emen t l eve l wh i l e t he s l ope ( n ) r ema ined t he
same . The re i s no s i gn i f i can t i nd i ca t i on t ha t t he s l ope (n ) had
an e f f ec t on t he compress i ve s t r eng th o f t he mo r ta r m i xes .
I n F i gu re 6 .30 , t he ove rs i ze pa r t i c l e s i ze d i s t r i bu t i on
pa rame te r s (D50 ) and (D10 ) a re p l o t t ed as a f unc t i on o f t he 28 -
day compress i ve s t r eng th i n o rde r t o f i nd t he i n f l uence o f
compress i ve s t r eng th on t he pa r t i c l es s i ze d i s t r i bu t i on .
010203040506070
0 20 40 60 80 100
Oversize Particle size distribution parameters (μm)
Com
pres
sive
Str
engt
h M
Pa
0%
10%
20%
35%
55%
D50 D10
F igu re 6 .30 Re la t i on be tween 28 -day compre ss ion s t reng th and
pa r t i c l e s i ze d i s t r i bu t i on pa rame te r s o f r ep l acemen t l eve l o f
gas i f i ca t i on ash
As t he ave rage pa r t i c l e s i ze becomes sma l l e r t he 28 -day
compress ion s t r eng th dec reases . As t he 10% l a rges t pa r t i c l e
s i ze fo r d i f f e ren t r ep lac emen t l eve l s become sma l l e r
compress i ve s t r eng ths a l so dec reases . I t i s howeve r
i n t e res t i ng t o no te t ha t t he re i s no c l ea r i nd i ca t i on t ha t t he
ave rage pa r t i c l e s i ze o r t he 10% l a rges t pa r t i c l e s i ze becomes
sma l l e r f o r d i f f e ren t r ep lacemen t l e ve l s . The ave rage pa r t i c l e
s i ze f o r t he d i f f e ren t r ep lac emen t l eve l s r ange be twe en 15µm
and 20µm, wh i l e t he 10% l a rges t pa r t i c l e s i ze r ange be tween
40µm an d 95µm. F rom the g raph t he re i s no op t imum l im i t f o r
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-38
bo th t he 50% and 10% l a rges t pa r t i c l e s i ze d i s t r i bu t i on
pa rame te rs .
6 .8 COMPA R ISON BE TWEEN MAN UFA CTURE D AND COMMER CIAL CE MENT
6 .8 .1 Mor ta r P r ism Co mpress ive S t reng th
The cemen t manu fac tu red i n t he l ab was compa red t o
commerc ia l l y ava i l ab l e CEM I 42 .5R . See Append i x I f o r a
summary o f s t reng ths . The cemen t manu fac tu red i n t he
l abo ra to r y was e i t he r i n t e rb l ended ( i n t e rb l end i n m i xe r ) o r
i n t e rg round ( i n t e rb l end i n ba l l m i l l and g round t oge the r ) f o r 2
hou rs w i th a 2 .5% gypsum con ten t . F i gu re 6 .31 i nd i ca tes t he
compress i ve s t r eng ths f o r i n t e rb l ended and i n t e rg round cemen t
manu fac tu red i n t he l ab and a commerc i a l l y ava i l ab l e CEM I
42 .5R . F rom the g raph i t i s obse rved t ha t i n te rg r i nd i ng cemen t
and gypsum ach ieved compress i ve s t r eng ths h i ghe r t han t he
CEM I 42 .5R , wh i l e i n t e rb l end ing ac h ieved l owe r compress i ve
s t r eng ths t han t he CEM I 42 .5R .
010203040506070
2 Days 7 Days 28 Days
Days
Com
pres
sive
Str
engt
h M
Pa
IB CEM+GYPSUM IG CEM +GYPSUM CEM I 42.5 R
F igu re 6 .31 Compress i ve s t r eng ths f o r manu fac tu red and
commerc i a l l y ava i l ab l e cemen t
F rom th e s t r eng th c l ass r equ i r emen ts i n Tab le 6 .12 t he
d i f f e rence can be obse rved i n t e rms o f s t r eng th . I n te rb l end ing
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-39
can be c l ass i f i ed as 42 .5N wh i l e i n te rg r i nd i ng i s c l ass i f i ed as
52 .5N .
Tab le 6 .12 a l so i nd i ca tes t he pe rcen tage o f 28 day s t r eng th
ga ined a f t e r 7 days , wh i ch i nd i ca tes t ha t i n t e rb l end ing and
i n t e rg r i nd i ng ach ieved a t l eas t 80% o f t he s t reng th a f t e r 7 days .
The CEM I 42 .5 R ach ieved on l y 68% o f i t s s t r eng th
deve lopmen t a f t e r 7 days . F rom the resu l t s i t i s c l ea r t ha t t he
i n t e rg round cemen t manu fac tu red i n t he l ab pe r f o rmed be t t e r
t han a commerc i a l l y ava i l ab l e 42 .5R . The i n t e rb l ended cemen t
manu fac tu red cemen t pe r f o rmed l i ke a 42 .5N bu t had a f as te r
s t r eng th deve lopmen t a f t e r 7 days t han t he 42 .5R .
Tab le 6 .12 S t reng th c l asses f o r d i f f e ren t r ep lacemen t l eve l s o f
gas i f i ca t i on ash
IB CEM + Gypsum
IG CEM + Gypsum CEM I 42.5R
Strength class 42.5 N 52.5 N 42.5 R
Percentage strength
development after 7 days
82% 80% 68%
6 .8 .2 F lexura l Mor ta r P r ism S t re ng ths
F igu re 6 .32 shows t he f l exu ra l s t r eng ths (Append i x I ) f o r
i n t e rb l ended and i n t e rg round cemen t manu fac tu red i n t he l ab
and a commerc ia l l y ava i l ab l e CEM I 42 .5N . F rom the g raph i t i s
obse rved t ha t i n te rg round cemen t ach ieved s im i l a r f l e xu ra l
s t r eng ths t han t he CEM I 42 .5N .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-40
02468
1012
2 Days 7 Days 28 DaysDays
Flex
ural
Str
engt
h M
Pa
IB CEM+GYPSUM IG CEM +GYPSUM CEM I 42.5 R
F igu re 6 .32 F lexu ra l s t r eng ths f o r manu fac tu red and
commerc i a l l y ava i l ab l e cemen t
Tab le 6 .13 g i ves a pe rcen tage o f t he compress i ve s t r eng th
ach ieved by t he f l exu ra l s t r eng th a f t e r 28 days . I n t e rb l end ing
ach ieved t he h i ghes t pe r cen tage o f f l e xu ra l s t r eng th compa red
t o compress i ve s t r eng th . The i n t e rg round and CEM I 42 .5R
m ixes ach ieved sma l l e r pe rcen tages bu t a l l t h ree o f t he m i xes
ach ieved a pe rcen tage h i ghe r t han 10% wh i ch i s expec ted . The
resu l t s i nd i ca te t ha t t he bo th t he i n te rb l ended and i n te rg round
cemen t pe r f o rmed s im i l a r t o t he commerc ia l l y ava i l ab l e CEM I
42 .5R .
Tab le 6 .13 Pe rcen tage o f compress i ve s t r eng th ach ieved f o r
d i f f e ren t r ep l acemen t l eve l s o f gas i f i ca t i on ash
IB CEM + Gypsum
IG CEM + Gypsum
CEM I 42.5R
Percentage of compressive
strength achieved
20% 16% 19%
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-41
6 .8 .3 Hea t o f Hyd ra t io n
F igu re 6 .33 shows t he ra te o f hea t deve lopmen t f o r t he
manu fac tu red and commerc i a l l y ava i l ab l e cemen t . F rom the
g raph i t i s obse rved t ha t t he cemen t manu fac tu red i n t he l ab
peak a t t he same t ime as t he CEMI 42 .5R bu t a t a l owe r hea t
evo lu t i on . A f t e r t h e f i r s t peak bo th t he m i xes dec rease w i t hou t
any shou lde rs wh i ch i nd i ca te f l a sh o r f a l se se t . The resu l t s
i nd i ca te t ha t t he cemen t manu fac tu red i n t he l ab pe r f o rmed
s im i l a r t o t he commerc i a l l y ava i l ab l e CEM I 42 .5R bu t l owe r
hea t o f hyd ra t i on t empe ra tu res i s obse rved f o r t he cemen t
manu fac tu red i n t he l ab .
0
0.25
0.5
0.75
1
1.25
1.5
1.75
2
0 5 9 14 18 23 27 32 36 41 45 50 54 59 63 68
Time (hours)
dQ/d
t (m
Wat
ts/g
.sec
)
CEM I 42.5
LAB CEM
F igu re 6 .33 Ra te o f hea t deve lopmen t f o r manu fac tu red and
commerc i a l l y ava i l ab l e cemen t
6 . 9 CONCLUSION
• I t i s obse rved t ha t t he gas i f i ca t i on ash , g r i nded sepa ra te
and i n t e rg round had s im i l a r pa r t i c l e s i ze d i s t r i bu t i ons .
The pa r t i c l e s i ze o f gas i f i ca t i on ash g round sepa ra te l y i s
cons ide rab l y f i ne r t han t ha t o f cemen t g round sepa ra te l y
f o r t he same t ime i n t e r va l . Th i s i nd i ca tes t ha t t he cemen t
c l i n ke r i s ha rde r t han t he gas i f i ca t i on ash c l i n ke r .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
6-42
• The pos i t i on pa rame te r (X o ) and t he re fo re t he pa r t i c l e
s i ze d i s t r i bu t i on dec rease as t he g r i nd i ng t ime i nc reases
f o r gas i f i ca t i on ash .
• I t seems as i f an op t imum g r i nd i ng t ime can be
es tab l i shed . Fo r bo th t he i n t e rg r i nd i ng and gas i f i ca t i on
ash t h i s op t imum seems t o be i n t he r eg ion o f 2 hou rs .
• The gas i f i ca t i on as h has no un ique s t r uc tu re and cou ld be
desc r i bed as angu la r .
• The XRF , XR D and chem ica l spec i f i ca t i on r esu l t s i nd i ca te
t ha t gas i f i ca t i on ash shou ld be accep tab le t o use as a
cemen t ex tende r i n conc re te .
• The compress i ve s t r eng th , f l e xu ra l s t r eng th , pa r t i c l e s i ze
and Ros in -Rammle r d i s t r i bu t i on pa rame te rs c l ea r l y
i nd i ca te tha t g r i nd i ng t ime shou ld no t be sho r t e r t han 2
hou rs f o r i n t e rb l end ing and i n t e rg r i nd i ng o f gas i f i ca t i on
ash and cemen t .
• I t can be deduced t ha t a 2 .5% gypsum add i t i on i s a good
ave rage t o use i n f u r t he r t es t i ng when hea t o f hyd ra t i on
and compress i ve s t r eng th a re cons ide red .
• The compress i ve s t r eng th , f l e xu ra l s t r eng th , pa r t i c l e s i ze
and Ros in -Ramml e r d i s t r i bu t i on pa rame te r s con f i rm t ha t
r ep l acemen t l eve l s o f gas i f i ca t i on ash shou ld r ange
be tween 10% and 35%.
• The cemen t manu fac tu red i n t he l abo ra to r y pe r f o rmed
s im i l a r i n s t r eng th deve lopmen t t o t he commerc i a l l y
ava i l ab l e CEM I 42 .5R bu t l owe r hea t o f hyd ra t i on
t empe ra tu res a re obse rved f o r t he cemen t manu fac tu red
i n t he l abo ra to r y .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
7-1
7. TEST RESULTS AND DISCUSSION ON CONCRETE TESTS
7 .1 INTRODUCTION
I n chap te r 7 , t he r esu l t s o f t he expe r imen ta l t es t s d i scussed i n
chap te r 5 on conc re te a re r ev i ewe d and ana l ysed t o exam ine
t he reac t i v i t y o f a gas i f i ca t i on ash when used i n conc re te .
The rea f t e r t he r esu l t s o f t he conc re te cas t a re i l l u s t r a ted and
d i scussed . The resu l t s i nc l ude s l ump , compress i on s t r eng th ,
t ens i l e s t r eng th , E - va lue , sh r i nkage , c reep , po ros i t y and
oxygen p e rmeab i l i t y t es t r e su l t s . The d i scuss ion o f t he r esu l t s
t akes i n to cons ide ra t i on t ha t t es t s we re conduc ted on a s i ng l e
se t o f samp les . L im i t a t i ons t o t he t es t i ng me thod w i l l be
d i scussed and poss ib l e imp rovemen ts w i l l be r ecomme nded .
7 .2 TESTS C OND UCT ED ON F RESH CONCRET E 7 .2 .1 S lump Tes t
The s l ump t es t r esu l t s ( as i nd i ca ted i n f i gu re 7 .1 ) i l l us t r a t e t ha t
t he conc re te m i x i n t e rb l ended w i t h f l y ash had t he h i ghes t
s l ump and t hus a h i gh workab i l i t y . I t i s expec ted t ha t due t o
t he f i l l e r e f f ec t s cha rac te r i s t i c o f f l y ash i t w i l l e xh ib i t a s l i gh t l y
l owe red pas te wa te r demand . Th i s i nc reases t he cohes i veness
o f t he m i x wh i ch i mp roves i t s wo rkab i l i t y (Ho l c im , 2005 ) . The
m ixes w i t h gas i f i ca t i on ash we re l ess wo rkab le . Resu l t s
i nd i ca te t ha t t he wa te r deman d o f conc re te con ta i n i ng
gas i f i ca t i on ash i s h i ghe r t han t ha t o f t he m i x i n t e rb l ended w i t h
f l y ash . The s l ump t es t r esu l t s i nd i ca te t ha t t he use o f
gas i f i ca t i on ash as cemen t ex tende r w i l l r esu l t s i n a reduc t i on
i n t he wo rkab i l i t y o f conc re te .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
7-2
0
40
80
120
160
200
IG IB FA IB GA
Mixes
Slum
p m
m
F igu re 7 .1 S lump t es t f o r conc re te m i xes
7 .3 STRENGTH TEST S 7 .3 .1 Concre te Cube Co mpress ion Tes t Resu l ts
F i gu re 7 .2 shows t he compress i ve s t r eng th o f t he d i f f e ren t
conc re te m i xes . The h i ghes t s t r eng th was ach ieved by t he
i n t e rg r i nded gas i f i ca t i on ash m i x , bu t t he s t r eng th d i f f e rence i s
no t g rea te r t han 5 MPa f o r a l l t he m i xes a f t e r 28 days ( see
Append i x J ) . The l owes t s t r eng ths we re ach ieved by t he
i n t e rb l end ing w i t h f l y ash . These resu l t s c l ea r l y i nd i ca te t ha t
t he use o f gas i f i ca t i on ash as cemen t ex tende r does no t have a
nega t i ve impac t on t he s t r eng th deve lopmen t o f conc re te .
A f t e r 7 days t he gas i f i ca t i on ash i n te rg r i nded ach ieves a h i gh
compress i ve s t r eng th . Th i s va l ue cou ld s t a t i s t i ca l l y be
cons ide red as an ou t l i e r bu t no t r ends can be conc luded f r om
the resu l t s as on l y one se t o f samp les we re tes ted . Th i s va l ue
v i s i b l y i nd i ca tes tha t mo re t es t i ng shou ld be done so t ha t
s t a t i s t i ca l conc lus i ons cou ld be d rawn abou t t he behav iou r o f
compress i ve s t r eng th o f gas i f i ca t i on .
The compress i ve s t r eng th t es t i s howeve r no t a good i nd i ca to r
o f conc re te du rab i l i t y as no d i r ec t r e l a t i onsh ip ex i s t s be tween
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
7-3
the two cha rac te r i s t i c s . The qua l i t y o f conc re te , i n t e rms o f
du rab i l i t y , shou ld t he re fo re no t be de duced f r om the
compress i ve s t r eng th , as i s o f t en the case i n t he cons t ruc t i on
i ndus t r y .
05
101520253035
24 hour 7 days 28 days
Time
Com
pres
sive
str
engt
h M
Pa
IG
IB FA
IB GA
F igu re 7 .2 Conc re te cubes compress ion s t r eng th r esu l t s
7 .3 .2 Tens i l e S t reng th Resu l ts
Theo re t i ca l l y t he tens i l e s t reng th i s expec ted t o be 10% o f t he
compress i ve s t r eng th . Resu l t s i n Tab le 7 .1 , shows t ha t t he
t ens i l e s t r eng th o f t he m i xe s was a l l app rox i ma te l y 3 MPa . A l l
o f t he m i xes had a f l e xu ra l s t r eng th t o compress i ve s t r eng th
compa r i son o f 10% to 12%. H ighe r t han 10% fo r t he
i n t e rb l end ing m i xes was due t o a l owe r compress i ve s t r eng th
t han t he i n t e rg r i nd i ng m ix . The f l exu ra l s t r eng th r esu l t s o f
gas i f i ca t i on ash , i n t e rg r i nded o r i n t e rb l ended was marg ina l l y
h i ghe r t han t he m i x i n t e rb l ended w i t h f l y ash . The t ens i l e
r esu l t s a re howeve r w i t h i n 0 .3 MPa o f each o the r and t he re fo re
t he d i f f e rence i s no t cons ide rab le . I n t e rb l end ing w i t h
gas i f i ca t i on ash has a s l i gh t l y h i ghe r t ens i l e s t r eng th t han t he
f l y ash .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
7-4
Tab le 7 .1 Tab le compa r i ng t ens i l e and compress i ve s t reng ths
Mixes Tensile strength MPa
Compression Strength MPa Comparison %
IG 3.3 31.5 10%
IB FA 3.02 26.7 11%
IB GA 3.35 28.0 12%
F rom F igu re 7 .3 , i t can be seen t ha t i n t e rb l end ing and
i n t e rg r i nd i ng w i t h gas i f i ca t i on ash ach ieved t he h i ghes t t ens i l e
s t r eng ths . These resu l t s i nd i ca te tha t t he use o f gas i f i ca t i on
ash as cemen t ex tende r does no t r esu l t s i n a r educ t i on i n t he
t ens i l e s t r eng th o f conc re te .
0
1
2
3
4
Mixes
Tens
ile s
tren
gth
MPa
IG
IB FA
IB GA
F igu re 7 .3 Tens i l e s t r eng th r esu l t s f o r conc re te m i xes
7 .4 DEFORMATION A ND V OLU ME C HA NGE OF CON CRE TE 7 .4 .1 E -va lue tes t resu l ts
The e l as t i c modu lus r ep res en t s t he ma te r i a l s t i f f ness o f t he
conc re te t o an imposed s t r ess . F i gu re 7 .4 shows t he ave rage o f
two resu l t s f o r each m ix . The resu l t s f o r t he E -va lue show tha t
i n t e rg r i nd i ng w i t h gas i f i ca t i on ash ach ieved t he h i ghes t
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
7-5
modu lus o f e l as t i c i t y . I n t e rb l end ing w i t h gas i f i ca t i on ash
ach ieved t he l owes t modu lus o f e l as t i c i t y .
0
10
20
30
40
50
Mixes
Mod
ulus
of E
last
icity
GPa
IGIB FA
IB GA
F igu re 7 .4 E -va lue t es t r esu l t s f o r conc re te m i xes
Gas i f i ca t i on ash i n t e rg r i nded ach ieved a h i ghe r mo du lus o f
e l as t i c i t y t han t h e i n t e rb l end ing m ixes ( see t ab le 7 .2 ) . Th i s
cou ld be due t o t he be t t e r i n t e r f ace o f t he pa r t i c l es a l r eady
m ix i ng when g r i nded t oge the r and due t o t he h i ghe r
compress i ve s t r eng th o f i n t e rg r i nd i ng . The re i s a cons tan t
d i f f e rence o f 2 GPa be tween each o f t he cy l i nde rs f o r a l l t h ree
m i xes . No t r ends can be conc luded f r om the resu l t s as on l y one
se t o f samp les we re t es ted . The h i gh s t i f f ness o f i n t e rg r i nd i ng
gas i f i ca t i on ash i nd i ca tes tha t mo re t es t i ng shou ld be done so
t ha t s t a t i s t i ca l conc lus i ons cou ld be d rawn abou t t he s t i f f ness
o f conc re te when gas i f i ca t i on ash i s i n t e rg r i nded w i t h cemen t .
These resu l t s i nd i ca te t ha t t he use o f gas i f i ca t i on ash as
cemen t ex tende r does no t have a de t r imen ta l e f f ec t on t he
s t i f f ness o f conc re te .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
7-6
Tab le 7 .2 E -va lu e resu l t s o f t he d i f f e ren t cy l i nde rs f o r t he
d i f f e ren t m i xes
Mix E-value Cylinder 1
E-value Cylinder 2
IG 38.8 GPa 40.3 GPa
IB FA 37.8 GPa 35.9 GPa
IB GA 35.4 GPa 33 GPa
7 .4 .2 Shr inkage and Creep Tes t
Sh r i nkage i s caused by d r y i ng t he re fo re f ac to r s t ha t con t r i bu te
t o t he d r y i ng o f conc re te such as r e l a t i ve hum id i t y , s i ze and
shape o f t he conc re te member as we l l as t he conc re te m i x
p ropo r t i ons and ma te r i a l s w i l l i n f l uence sh r i nkage .
Tab le 7 .3 i nd i ca tes t he sh r i nkage , c reep and spec i f i c c reep f o r
each o f t he m i xe s a f t e r 309 days . F rom the resu l t s i t i s
obse rved t ha t i n te rg r i nd i ng and i n t e rb l end ing o f gas i f i ca t i on
ash ach ieved h i ghe r sh r i nkage , c reep and spec i f i c c reep
resu l t s t han t he i n t e rb l ended f l y ash m ix . Thes e d i f f e rences a re
on l y ma rg ina l .
Tab le 7 .3 Sh r i nkage , C reep and Spec i f i c C reep Resu l t s f o r t he
d i f f e ren t m i xes
MIX Shrinkage (microstrain)
Creep (microstrain)
Specific Creep (microstrain/Mpa)
IG GA 413.4 830.7 201.1 IB FA 326.8 643.7 169.8
IB GA 378.0 783.5 184.6
P rev i ous s tud ies conduc ted by Badenho rs t ( 2003 ) showed t ha t
f o r a 70 /30 FA b l ended cemen t i t i s expec ted t ha t f o r d i f f e ren t
agg rega te t he sh r i nkage d i f f e r s . A do lom i t e sand and g ran i t e
s t one was used i n t he m i x des ign o f t he conc re te f o r a l l t h ree
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
7-7
m ixes . G ran i t e has an expec ted sh r i nkage o f 500 m ic ros t r a i n
wh i l e do lom i t e has an expec ted sh r i nkage o f 300 m ic ros t r a i n .
The resu l t s o f t he t h ree m ixes f a l l i n t h i s r ange and t hus t he
d i f f e rence i n sh r i nkage fo r t he m i xes i s no t cons ide rab le .
F i gu res 7 .5 , 7 . 6 and 7 .7 i nd i ca te t he sh r i nkage and c reep f o r
each o f t he t h ree m ixes . The resu l t s f o r sh r i nkage i nd i ca te t he
gas i f i ca t i on ash d i d no t sh r i nk s i gn i f i can t l y mo re t han f l y ash .
IG GA73 kN Load; 55% to 60% RH; 25oC
0100200300400500600700800900
1000
0 50 100 150 200 250 300 350
Time (days)
Def
orm
atio
n (m
icro
stra
in)
CreepCreepShrinkage
F igu re 7 .5 Sh r i nkage and c reep resu l t s f o r i n t e rg round
gas i f i ca t i on ash m ix
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
7-8
IB FA67 kN Load; 55% to 60% RH; 25oC
0100200300400500600700800900
1000
0 50 100 150 200 250 300 350
Time (days)
Def
orm
atio
n (m
icro
stra
in)
Creep
Creep
Shrinkage
F igu re 7 .6 Sh r i nkage and c reep resu l t s f o r i n te rb l ended f l y ash
m ix
IB GA 75 kN Load; 55% to 60% RH; 25oC
0100200300400500600700800900
1000
0 50 100 150 200 250 300 350
Time (days)
Def
orm
atio
n (m
icro
stra
in) Creep
Creep
Shrinkage
F i gu re 7 .7 Sh r i nkage and c reep resu l t s f o r i n t e rb l ended
gas i f i ca t i on ash m ix
C reep o f conc re te i s l oad i nduced , and i s i n f l uenced by f ac to r s
assoc ia ted w i t h t he app l i ca t i on o f l oad and the ab i l i t y o f t he
conc re te t o w i t hs tand t he l oad . The po ten t i a l o f t he conc re te t o
c reep i s de te rm ined by m i x ma te r i a l s and p ropo r t i ons o f t he
conc re te .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
7-9
Tab le 7 .3 i nd i ca te t ha t i n t e rg round and i n t e rb l ended
gas i f i ca t i on ash m ixes had h i ghe r c reep va lues t han t he
i n t e rb l ended f l y ash m ix . T he d i f f e rence i n t he c reep va lues a re
howeve r no t cons ide rab le ( see f i gu re 7 .5 , 7 . 6 and 7 .7 ) . The
resu l t s f o r c reep i nd i ca te t he gas i f i ca t i on ash d i d no t c reep
s i gn i f i can t l y mo re t han f l y ash .
F i gu re 7 .8 i nd i ca te t he spec i f i c c reep (See Append i x K ) f o r t he
t h ree m ixes . I t i s obse rved t ha t ove r t ime t h e spec i f i c c reep f o r
t he t h ree m ixes i s app rox i ma te l y t h e same . The spec i f i c c reep
resu l t s i nd i ca te tha t gas i f i ca t i on as h has a spec i f i c c reep
s im i l a r t o f l y ash .
55% to 60% RH; 25oC
0
50
100
150
200
250
300
0 50 100 150 200 250 300 350
Time (days)
Spec
ific
Cre
ep
(mic
rost
rain
/ M
Pa)
IG GA
IB FAIB GA
F igu re 7 .8 Spec i f i c c reep resu l t s f o r t he t h ree d i f f e ren t m i xes
7 .5 DURABIL ITY TEST S 7 .5 .1 Poros i ty Tes t Resu l ts
I t can be obse rved f r om F i gu re 7 .7 t ha t f o r i n t e rb l end ing t he
po ros i t y o f t he gas i f i ca t i on ash was l owe r t han f l y ash . Th i s i s
due t o a f i ne r pa r t i c l e s i ze o f t he gas i f i ca t i on ash t han t he f l y
ash , wh i ch r esu l t s i n a mo re even d i s t r i bu t i on o f so l i d pa r t i c l es
i n t he conc re te .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
7-10
The conc re te m i x i n t e rb l ended w i t h f l y ash has t he h i ghes t
po ros i t y , wh i ch shows tha t t he cemen t pa r t i c l es d i d no t
d i spe rse un i f o rm l y t h rough the wa te r r esu l t i ng i n
agg lomera t i ons and l eav i ng l a rge spaces wh i ch do no t con ta i n
cemen t . These spaces f o rm cap i l l a r y po re s and en t ra i n a i r .
The resu l t o f t h i s i s a l owe r s t r eng th o f t he conc re te . The
i n t e rg r i nd i ng w i t h f l y ash had a f i ne r pa r t i c l e s i ze and resu l t s i n
a l owe r po ros i t y . I n t e rb l end ing w i t h gas i f i ca t i on as h had a
s l i gh t l y h i ghe r po ros i t y t han t he i n t e rg r i nd i ng w i t h gas i f i ca t i on
ash ; t h i s cou ld be due t o be t t e r i n t e r l ock i ng o f pa r t i c l es
g r i nded toge the r . See Append i x L f o r Po ros i t y summary .
The d i f f e rence i n po ros i t y be tween a l l t h ree m ixes i s be tween
15% and 16%. Po ros i t y va l ues (B r i t i sh Conc re te Soc ie t y , 2000 )
f o r a h i gh l y po rous conc re te i s g rea te r t han 15%. A l t h ree o f
t he m ixe s f a l l i n to t h i s ca tego ry and t hus t he d i f f e rence i n
r esu l t s i s om iss i b l e . The resu l t s i nd i ca te t ha t t he use o f
gas i f i ca t i on ash as cemen t ex tende r does no t r esu l t s i n an
i nc rease i n po ros i t y . I t i s t he re fo re an t i c i pa ted t ha t t he
conc re te con ta i n ing gas i f i c a t i on ash w i l l be no l ess du rab le
t han conc re te cu r ren t l y man u fac tu red .
0%
6%
12%
18%
Mixes
Poro
sity
% IG
IB FAIB GA
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
7-11
F igu re 7 .7 Po ros i t y r esu l t s o f conc re te m i xes
7 .5 .2 Ox ygen Permeab i l i t y Tes t Resu l ts
The resu l t s o f t he pe rmeab i l i t y t es t (as i nd i ca ted i n f i gu re 7 .8 )
show tha t t he t ype o f ash used d i d no t a f f ec t t he pe rmeab i l i t y
o f m i xes . The m ix i n t e rb l ended w i t h f l y ash ac h ieved the l owes t
pe rmeab i l i t y . H igh pe rmeab i l i t y i s due t o a poo r qua l i t y o f
cemen t pas te -agg rega te i n te r f ace . F l y ash has t he e f f ec t o f
r educ ing t he pe rmeab i l i t y , wh i ch i s obse rved f r om the resu l t s .
I n t e rg r i nd i ng had t he h i ghes t pe rmeab i l i t y and wou ld abso rb
t he mos t wa te r . See Append i x M f o r Pe rmeab i l i t y ca l cu l a t i ons .
0
2E-21
4E-21
6E-21
8E-21
1E-20
1.2E-20
Mixes
Perm
eabi
lity
(m/s
)
IG
IB FA
IB GA
F igu re 7 .8 Oxygen pe rmeab i l i t y t es t resu l t s f o r conc re te m i xes
Pe rmeab i l i t y va l ues (B r i t i sh Conc re te Soc ie t y , 2000 ) f o r a good
qua l i t y conc re te w i t h a l ow pe rmea b i l i t y i s sma l l e r t han 2 x 10 -
1 8 and a l l o f t he resu l t s f a l l i n t o t h i s ca tego ry . OP I va l ues as
seen i n F i gu re 7 .9 i nd i ca te an exce l l en t c l ass o f du rab i l i t y f o r
conc re te w i t h a g rea te r t han 10 OP I (A lexande r , 1999 ) . These
resu l t s i nd i ca te tha t t he use o f gas i f i ca t i on ash i n conc re te
ach ieves a l ow pe rmeab i l i t y and a du rab le conc re te can be
expec ted .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
7-12
0
6
12
18
24
Mixes
Oxy
gen
perm
eabi
lity
inde
xIG
IB FA
IB GA
F igu re 7 .9 Oxygen pe rmeab i l i t y i ndex resu l t s f o r t he conc re te
m ixes .
7 . 6 CONCLUSION
• The use o f gas i f i ca t i on as h as a cemen t ex tende r i n
conc re te wou ld have eco log i ca l and econom ica l bene f i t s
i n t he cemen t i ndus t r y .
• The s l ump t es t r esu l t s i nd i ca te t ha t t he use o f
gas i f i ca t i on ash as cemen t ex tende r w i l l r esu l t s i n a
r educ t i on i n t he wo rkab i l i t y o f conc re te .
• The use o f gas i f i ca t i on ash as cemen t ex tend e r does no t
have a n ega t i ve impac t on t he s t r eng th deve lopmen t o f
conc re te . The re was no reduc t i on i n t he t ens i l e s t r eng th
o f conc re te .
• The use o f gas i f i ca t i on ash as cemen t ex tend e r does no t
have a de t r imen ta l e f f ec t on t he s t i f f ness o f conc re te .
• The resu l t s f o r sh r i nkage i nd i ca te t he gas i f i ca t i on ash d i d
no t sh r i nk s i gn i f i can t l y mo re t han f l y ash . C reep resu l t s
i nd i ca te tha t gas i f i ca t i on ash d i d no t c reep s i gn i f i can t l y
mo re t han f l y ash . The spec i f i c c reep resu l t s i nd i ca te tha t
gas i f i ca t i on ash has a spec i f i c c reep s im i l a r t o f l y ash .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
7-13
• The resu l t s i nd i ca te t ha t t he use o f gas i f i ca t i on ash as
cemen t ex tende r does no t r esu l t s i n an i nc rease i n
po ros i t y . I t i s t he re fo re an t i c i pa ted t ha t t he conc re te
con ta i n i ng gas i f i ca t i on ash w i l l be no l ess du rab le t han
conc re te cu r ren t l y manu fac tu red .
• The use o f gas i f i ca t i on ash i n conc re te ach ieves a l ow
pe rmeab i l i t y and a du rab le conc re te can be expec ted .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
8-1
8. CONCLUSIONS AND RECOMMENDATIONS 8 .1 CONCLUSIONS
The a im o f t he r esea rch i s f u l f i l l ed and exp la i ned by g i v i ng
cons ide ra t i on t o each o f t he f o l l ow ing conc lus i ons .
I nves t i ga t i ng t he phys i ca l , chemica l and m ine ra l og i ca l
compos i t i on o f a gas i f i ca t i on ash samp le had t he fo l l ow ing
resu l t s :
• The gas i f i ca t i on as h has no un ique s t r uc tu re and cou ld be
desc r i bed as angu la r .
• The chem ica l and m i ne ra l og i ca l compos i t i on o f
gas i f i ca t i on ash i nd i ca tes t ha t t he ash have s im i l a r
e l emen ts t han f l y ash and i s w i t h i n t he a l l owab le r ange
f o r use as a cemen t ex tende r i n cemen t and conc re te .
• The phys i ca l p rope r t i es o f gas i f i ca t i on ash i nd i ca ted tha t
t he gas i f i ca t i on ash , g round sepa ra te and i n t e rg round
w i t h cemen t i n t he ba l l m i l l had s im i l a r pa r t i c l e s i ze
d i s t r i bu t i ons . The re i s a cons ide rab le d i f f e rence i n
pa r t i c l e s i ze be tween t he gas i f i ca t i on ash and cemen t
g round sepa ra te l y f o r t h e same t ime i n te r va l . Th i s
i nd i ca tes t ha t t he cemen t c l i n ke r i s ha rde r t han t he
gas i f i ca t i on ash c l i n ke r .
• The pos i t i on pa rame te r (X o ) and t he re fo re t he pa r t i c l e
s i ze d i s t r i bu t i on dec rease as t he g r i nd i ng t ime i nc reases
f o r gas i f i ca t i on ash .
I nves t i ga t i ng t he phys i ca l p rope r t i es o f cemen t manu fac tu r i ng
w i t h spec i f i c r e f e rence t o g r i nd i ng t ime , t he op t im i sa t i on o f
gypsum, spec i f i c su r f ace a rea and pa r t i c l e s i ze d i s t r i bu t i on had
t he f o l l ow ing resu l t s :
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
8-2
• I t seems as i f an op t imum g r i nd i ng t ime can be
es tab l i shed . Fo r bo th t he i n t e rg r i nd i ng and gas i f i ca t i on
ash t h i s op t imum seems t o be i n t he r eg ion o f 2 hou rs .
• The compress i ve s t r eng th , f l e xu ra l s t r eng th , pa r t i c l e s i ze
and Ros in -Rammle r d i s t r i bu t i on pa rame te r s c l ea r l y
i nd i ca te than g r i nd i ng t ime shou ld no t be sho r t e r t han 2
hou rs f o r i n t e rb l end ing and i n t e rg r i nd i ng o f gas i f i ca t i on
ash and cemen t .
• I t can be deduced t ha t a 2 .5% gypsum add i t i on i s a good
ave rage t o use i n f u r t he r t es t i ng when hea t o f hyd ra t i on
and compress i ve s t r eng th i s cons ide red .
The e f f ec t o f r ep l acemen t l eve l on t he p rope r t i es o f
i n t e rb l ended and i n t e rg round gas i f i ca t i on ash and cemen t
shows t ha t :
• The compress i ve s t r eng th , f l e xu ra l s t r eng th , pa r t i c l e s i ze
and Ros in -Ramml e r d i s t r i bu t i on pa rame te rs con f i rm tha t
r ep l acemen t l eve l s o f gas i f i ca t i on ash shou ld r ange
be tween 10% and 35%.
• The cemen t manu fac tu red i n t he l ab pe r f o rmed s im i l a r i n
s t r eng th deve lopmen t t o t he comme rc i a l l y ava i l ab l e CEM
I 42 .5R bu t l owe r hea t o f hyd ra t i on t empe ra tu res i s
obse rved f o r t he cemen t ma nu fac tu red i n t he l ab .
• I n t e rg r i nd i ng o f gas i f i ca t i on ash and cemen t i n t he ba l l
m i l l i s i n my op in i on be t t e r t han i n t e rb l end ing gas i f i ca t i on
ash and cemen t i n t he m i xe r .
The e f f ec t o f i n t e rb l ended and i n t e rg round gas i f i ca t i on ash and
cemen t on t he sho r t and l ong t e rm p rope r t i es o f conc re te had
t he f o l l ow ing resu l t s :
• The use o f gas i f i ca t i on as h as a cemen t ex tende r i n
conc re te wou ld have eco log i ca l and econom ica l bene f i t s
i n t he cemen t i ndus t r y .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
8-3
• The s l ump t es t r esu l t s i nd i ca te t ha t t he use o f
gas i f i ca t i on ash as cemen t ex tende r w i l l r esu l t s i n a
r educ t i on i n t he wo rkab i l i t y o f conc re te .
• The use o f gas i f i ca t i on ash as cemen t ex tend e r does no t
have a n ega t i ve impac t on t he s t r eng th deve lopmen t o f
conc re te . The re was no reduc t i on i n t he t ens i l e s t r eng th
o f conc re te .
• The use o f gas i f i ca t i on ash as cemen t ex tend e r does no t
have a de t r imen ta l e f f ec t on t he s t i f f ness o f conc re te .
• The resu l t s f o r sh r i nkage i nd i ca te t he gas i f i ca t i on ash d i d
no t sh r i nk s i gn i f i can t l y mo re t han f l y ash . C reep resu l t s
i nd i ca te tha t gas i f i ca t i on ash d i d no t c reep s i gn i f i can t l y
mo re t han f l y ash . The spec i f i c c reep resu l t s i nd i ca te tha t
gas i f i ca t i on ash has a spec i f i c c reep s im i l a r t o f l y ash .
The e f f ec t o f t he gas i f i ca t i on ash on t he du rab i l i t y o f conc re te
showed :
• The use o f gas i f i ca t i on ash as cemen t ex tend e r does no t
r esu l t s i n an i n c rease i n po ros i t y . I t i s t he re fo re
an t i c i pa ted t ha t t he conc re te con ta i n i ng gas i f i ca t i on ash
w i l l be no l ess du rab le t han conc re te cu r ren t l y
manu fac tu red .
• The use o f gas i f i ca t i on ash i n conc re te ach ieves a l ow
pe rmeab i l i t y and a du rab le conc re te can be expec ted .
• Gas i f i ca t i on ash can be used as a cemen t ex tended i n
conc re te .
8 .2 REC OMMENDATI O NS
• The env i r onmen ta l impac t o f dec reas ing CO 2 i n t he
manu fac tu r i ng o f cemen t can bene f i t f r om us ing
gas i f i ca t i on ash as a cemen t ex tende r .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
8-4
• The use o f gas i f i ca t i on as h as a cemen t ex tende r i n
conc re te i s h i gh l y r ecommended due t o cha rac te r i s t i c s
l i ke i nc reased s t r eng th deve lo pmen t and reduced
pe rmeab i l i t y .
• The e f f ec t o f va r i ab i l i t y i n chemica l p rope r t i es o f
gas i f i ca t i on ash shou ld be fu r t he r i nves t i ga ted .
• The e f f ec t o f adm ix tu res on gas i f i ca t i on ash cou ld
i n f l uence t he wa te r demand o f conc re te and cause
conc re te t o be expens i ve .
• Long t e rm t es t i ng shou ld be done on gas i f i ca t i on ash t o
de te rm ine t he e f f ec t on conc re te du rab i l i t y .
• Tes t i ng shou ld be repea ted on gas i f i ca t i on ash t o
de te rm ine a t r end f o r t he behav io r o f gas i f i ca t i on ash
when used as a cemen t ex t ende r i n conc re te .
• The g r i nd i ng t imes and resu l t s a re no t necessa r i l y t he
on l y answe r s i nce t he l abo ra to r y equ ipmen t has a
i n f l uence on t h i s .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
9-1
9. REFERENCES
ACI Commi t t ee 23 2 .1R-94 . Use o f Na tu ra l Pozzo lans i n
Conc re te . AC I Jou rna l , Feb rua ry 1995 ,
Add i s , B . J . and Owens , G . 2001 . Fu l t on ’ s Conc re te
Techno logy . E igh t Ed i t i on . Ceme n t and Conc re te
I ns t i t u t e . M id rand , Sou th A f r i ca .
A l exande r , M .G Mackechn ie , J .R and Ba l l im , Y . Gu id e
t o t he use o f du rab i l i t y i ndexes f o r ach iev i ng du rab i l i t y
i n conc re te s t r uc tu res . Un i ve r s i t y o f Cape Town and
Un i ve rs i t y o f W i twa te r s rand . Resea rch Monog ra ph
No .2 . Cape Town . 1999 .
Amer i can Coa l Ash Assoc ia t i on . 1997 . Coa l combus t i on
P roduc t -P roduc t i on and Use . A lexand r i a . V i r g i n i a .
ASTM C 469 -02 . S tanda rd t es t me thod f o r s t a t i c
modu lus o f e l as t i c i t y and po i sson ’ s r a t i o o f conc re te i n
compress i on . Wes t Conshohocken . Amer i can Soc ie t y
f o r Tes t i ng and Ma te r i a l s . 2002 .
ASTM C 512 -02 . S tanda rd t es t me thod f o r C reep o f
Conc re te i n Comp ress ion . Amer i can Soc ie t y f o r Tes t i ng
Ma te r i a l s . Wes t Conshohocken . Pennsy l van ia . 2002 .
ASTM C 1861 -97 . S tanda rd Gu ide f o r Use o f Coa l
Combus t i on By -P roduc t s i n S t ruc tu ra l F i l l s . Amer i can
Soc ie t y f o r Tes t i ng Ma te r i a l s . Wes t Conshohocken .
Pennsy l van ia . 2002 .
Babcock and W i l cox . 1978 . S team. I t s Gene ra t i on and
Use . New Yo rk , NY .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
9-2
Badenho rs t , S . 2003 . A C r i t i ca l rev i ew o f conc re te
d r y i ng sh r i nkage , t es t me th ods , f ac to r s i n f l uenc ing and
sh r i nkage p red i c t i on . Johannesbug . Un i ve r s i t y o f t he
W i twa te r s rand . Ju l y 2003 . (MSc P ro j ec t Repo r t ) .
Ba l l im , Y . 1999 . Loca l i s i ng i n t e rna t i ona l conc re te
mode l s – t he case o f c reep and sh r i nkage p red i c t i on .
P roceed ings o f t he 5 t h I n t e rna t i ona l con fe rence on
conc re te t echno logy f o r deve lop ing coun t r i es . New
De lh i . Vo lume 1 . P t 7 . Nove mber 1999 . pp 66 -78 .
Bha t t y , J . I . M i l l e r , F .M . and Kosma tka , S .H . 2004 .
I nnova t i ons i n Po r t l and Cemen t Manu fac tu r i ng .
Po r t l and Cemen t Assoc ia t i on . I l l i no i s .
Bouzoubaâ , N . Zhang , M .H . B i l odeau , A . and Ma lho t ra ,
V .M . 19 97 . The e f f ec t o f g r i nd i ng on t he phys i ca l
p rope r t i es o f f l y ashes and a Po r t l and cemen t c l i n ke r .
Cemen t and Conc re te Resea rch . Vo lume 2 7 , Numb er .
12 . pp 1862 – 1874 .
B r i t i sh Conc re te Soc ie t y . 2000 . B r i t i sh Conc re te
Soc ie t y t echn i ca l r epo r t numbe r 54 . D iagnos i s o f
de te r i o ra t i on i n conc re te s t r uc tu res . I den t i f i ca t i on o f
de fec t s , eva lua t i on and deve lopmen t o f r emed ia l
ac t i on . Conc re te Soc ie t y . London .
B rown , J .H . 1982 . The s t r eng th and wo rkab i l i t y o f
conc re te w i t h PFA subs t i t u t i on . I n P roceed ings ,
I n t e rna t i ona l Sympos ium on t he Use o f PFA i n
Conc re te . Un i ve r s i t y o f Lee ds , UK . Ap r 14 -1 6 . Ed i t ed
by J .G . Cab re ra and A .R . Cusens . Depa r tmen t o f C i v i l
Eng inee r i ng . Un i ve r s i t y o f Leeds , Leeds , UK . pp 151 -
161 .
Bye , G . C . Po r t l and cemen t . 1999 . Compos i t i on ,
p roduc t i on and p rope r t i es . 2 n d ed i t i on . Thomas Te l f o rd .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
9-3
Ca re t t e , G .G and Ma lho t ra , V .M . 1986 . Cha rac te r i za t i on
o f Canad ian f l y ashes and the i r r e l a t i ve pe r f o rmance i n
conc re te . Ene rgy , M ines and Resou rces Canada .
CENMET Repo r t 86 -6E . O t t awa . ON.
Ch indap ras i r t , P . Homwu t t i wong , S and S i r i v i va tnanon ,
V . 2004 . I n f l uence o f f l y ash f i neness on s t r eng th ,
d r y i ng sh r i nkage and su lpha te r es i s t ance o f b l ended
cemen t mo r ta r . Cemen t and Conc re te Resea rch .
Vo lume 34 . pp 1087 – 1092 .
Dav i s , R .E Ca r l son , R .W Ke l l y , J .W and Dav i s , H .E .
1937 . P rope r t i es o f cemen ts and conc re tes con ta i n i ng
f l y ash . Jou rna l o f t he Amer i can Conc re te I ns t i t u t e ,
Vo lume 33 , pp 577 -612 .
D iamond , S . and Lopez -F lo res , F . 1981 . On t he
d i s t r i bu t i on be tween phys i ca l and chem ica l
cha rac te r i s t i c s be tween l i gn i t i c and b i t um inous f l y
ashes . P roceed ings , Symp os ium on E f f ec t s o f F l y Ash
I nco rpo ra ted i n Cemen t a nd Conc re te . Ed i t ed by S .
D iamond . Ma te r i a l s Resea rch Soc ie t y . Bos ton , MA . pp
34 -44 .
E rdogdu , K . Tokyay M . and Tü rke r , P . 1999 .Compar i son
o f i n t e rg r i nd i ng and sepa ra te g r i nd i ng f o r t he
p roduc t i on o f na tu ra l pozzo lan and GBFS- i nc o rpo ra ted
b l ended cemen ts . Cemen t and conc re te r esea rch ,
Vo lume 29 , pp 743 -746 .
Esca lan te -Ga rc i a , and Sha rp , J .H . 2004 . The chem ica l
compos i t i on and m ic ros t r uc tu re o f hyd ra t i on p roduc t s i n
b l ended cemen ts . Cemen t and conc re te compos i t es ,
Vo lume 26 , pp 967 -976 .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
9-4
F r i g i one , G . 1983 . Gypsum i n Ce men t . I n : Ghosh SN
ed . Ceme n t Techno logy . Pe rgamon P ress .New Yo rk . pp
485 -535 .
F r i g i one , G . and Mara , S . 1976 . Re la t i onsh ip be tween
pa r t i c l e s i ze d i s t r i bu t i on and compress i ve s t r eng th i n
P ro t l and Cemen t . Cemen t and Conc re te Resea rch .
Vo lume 6 . pp 113 -128 .
Ghosh , R .S . and T imusk , J . 1981 . C reep o f f l y ash
conc re te . Jou rna l o f t he Amer i can Conc re te I ns t i t u te .
Vo lume 87 . pp 351 -357 .
G r i eve , G .R .H . 1991 . The i n f l uence o f two So u th
A f r i can f l y ashes on t he eng inee r i ng p rope r t i es o f
conc re te . PhD thes i s . Johannesbu rg . Un i ve r i s t y o f t h e
W i twa te r s rand .
Hec t , N .L . and Du va l l , D .S . 1975 . Cha rac te r i sa t i on and
U t i l i za t i on o f Mun i c i pa l and U t i l i t y S l udges and Ashes :
Vo lume I I I –U t i l i t y Coa l Ash . Na t i ona l Env i r onmen ta l
Resea rch Cen te r . U .S . Env i r o nmen ta l P ro tec t i on
Agency .
Ho l c im . 2005 . Ma te r i a l s Handbook . Ho l c im Sou th
A f r i ca .
I l l s t on , J .M . and Domone , P .L . J . 2001 . Cons t ruc t i on
Ma te r i a l s . The i r na tu re and behav iou r . Th i rd Ed i t i on .
Spon P ress , London .
Josh i , R .C . 1982 . E f f ec t o f coa rse f rac t i on (+ #325 ) o f
f l y ash on conc re te p rope r t i es . I n P roceed ings , 6 t h
I n t e rna t i ona l Symp os ium on F l y Ash U t i l i za t i on . Reno ,
NV . Ma rc h 1982 . U .S . Dep a r tmen t o f t he Env i r onmen t .
Wash ing ton , DC . DOE/ MET C/82 -52 . pp 77 -85 .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
9-5
K rüge r , J .E . 1999 . Gu ide 2 : O r i g i n , H i s t o r y and
P rope r t i es o f Sou th A f r i can F l y As h and Po r t l and F l y
Ash Cemen ts . Gu ides on the use o f Sou th A f r i can f l y
ash as a cemen t e x tende r . The Sou th A f r i can Coa l As h
Assoc ia t i on , Sou th A f r i ca .
Lane , R .O . and Bes t , J .F . 1982 .P rope r t i es and use o f
f l y ash on Po r t l and cemen t conc re te . Conc re te
I n t e rna t i ona l . Vo lume 4 , Nu mber 7 . pp 81 -92 .
Lea FM. 1970 . Chem is t r y o f cemen t and conc re te . 4 t h
ed . Edward A rno ld Pub l i she rs L td . G rea t B r i t a i n .
Lee , S .H . K im , H . J . Saka i , E and Da imon , M . 2003 .
E f f ec t o f pa r t i c l e s i ze d i s t r i bu t i on o f f l y ash -cemen t
sys tem o n t he f l u i d i t y o f cemen t pas tes . Cemen t and
conc re te r esea rch , Vo lume 33 , pp 763 -768 .
Le r ch , W . 1946 . The i n f l uence o f gypsum on t h e
hyd ra t i on and p ro pe r t i es o f Po r t l and cemen t pas tes .
PCA Bu l l e t i n . Number 12 .
Loche r , F .W. Sp rung , S . and Ko r f , P . 1973 . The e f f ec t
o f pa r t i c l e s i ze d i s t r i bu t i on on t he s t r eng th o f Po r t l and
cemen t . Zemen t -Ka l k -G ips . Vo lume 26 . pp 349 -355 .
Massazza , F . 1998 . Chem ica l ana l ys i s o f Po r t l and
cemen ts . Chap te r 4 : Lea ’ s Chem is t r y o f Cemen t an d
Conc re te , Fou r t h Ed i t i on , Ed i t ed by He w le t t , P .C .
A rno ld , London .
Ma lho t ra , V .M . an d Meh ta , P . J . 1996 . Pozzo lan i c and
Cemen t i t i ous Ma te r i a l s . F i r s t Ed i t i on . Go rdon and
B reach Pub l i she rs , Ams te rdam.
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
9-6
Me tha , P .K . 1989 . Pozzo lan i c and cemen t i t i ous by -
p roduc t s i n conc re te – Ano the r l ook . P roceed ings , 3 r d
CANMET/ ACI I n t e rna t i ona l Con fe rence on the use o f
F l y Ash , S i l i ca Fume , S lag and O the r M i ne ra l By -
P roduc t s i n Conc re te , T rondhe im , No rway . J une 18 -23 .
Ed i t ed by V .M . Ma lho r t a . Amer i can Conc re te I ns t i t u t e .
De t ro i t , M I . Spec ia l Pub l i ca t i on SP-114 , Vo lume 1 , pp
1 -43 .
Na i k , T .R . and Ra mme, B . W. 1990 . E f f ec t o f h i gh - l ime
f l y ash con ten t on wa te r demand , t ime o f se t and
compress i ve s t r eng th o f conc re te . AC I Ma te r i a l s
Jou rna l . Vo lume 87 . pp 619 -626 .
Nev i l l e , A .M . 19 95 . P rope r t i es o f Conc re te . Fou r t h
Ed i t i on . Longman Group L td . London .
Newman , J . 2003 . Advanced conc re te techno logy .
E l sev i e r L td .
O lo runsogo , F .T . 1990 . E f f ec t o f pa r t i c l e s i ze
d i s t r i bu t i on o f g round g ranu la ted b l as t f u rnac e s l ag on
some p rope r t i es o f s l ag cemen t mo r ta r . PhD thes i s ,
Un i ve r s i t y o f Leeds .
Owens , P .L . 1979 . F l y ash and i t s usage i n conc re te .
Conc re te : The Jou rna l o f t he Conc re te Soc ie t y . Vo lume
13 . pp 21 -26 .
Pandey , S .P . 1 983 . The Pa r t i c l e S i ze D i s t r i bu t i on
Ana l ys i s : Sc i ence and App l i ca t i ons i n Ceme n t
Techno logy . I n : Ghosh SN ed . Cemen t Techno logy .
Pe rgamo n P ress .New Yo rk . pp 735 -775 .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
9-7
Ros in , P . and Ra mmle r , E . 1933 . The l aws gove rn i n g
t he f i neness o f powde red coa l . Jou rna l o f t he I ns t i t u te
o f Fue l . Vo lume 7 . pp 29 -33 .
Sandbe rg , P . 2005 . The us e o f I so the rma l ca l o r ime t r y
t o op t im i se cemen t su l pha te Pa r t 1 – Ceme n t w i t hou t
adm ix tu res . I n t e rna l Documen t . G race Cons t ruc t i on
P roduc t s .
SANS 14 91 /SABS 1491 :1989 . Po r t l and cemen t ex tende rs ,
Pa r t 1 : G round g ranu la ted b l as t f u rnace s l ag , Pa r t 2 : S i l i ca
f ume , Pa r t 3 : F l y ash . Sou th A f r i can Bu reau o f S tanda rds .
P re to r i a .
SANS 50 196 -1 /SABS 196 -1 :1994 . Me thods o f t es t i ng
cemen t , Pa r t 1 : De te rm ina t i on o f s t r eng th . Sou th
A f r i can Bu reau o f S tanda rds . P re to r i a .
SANS 50 196 -2 /SABS 196 -1 :1994 . Me thods o f t es t i ng
cemen t , Pa r t 1 : Su lphu r t r i o x i de con ten t and l oss on
i gn i t i on . Sou th A f r i can Bu reau o f S tanda rds . P re to r i a .
SANS 50 196 -3 /SABS 196 -1 :1994 . Me thods o f t es t i ng
cemen t , Pa r t 1 : Soundness . Sou th A f r i can Bu reau o f
S tanda rds . P re to r i a .
SANS 5 0197 -1 /SABS 197 -1 :2000 . Cemen t Pa r t 1 :
Compos i t i on , spec i f i ca t i on and con fo rm i t y c r i t e r i a f o r
common cemen ts . Sou th A f r i can Bu reau o f S tanda rds .
P re to r i a .
SANS 5 862 /SABS SM 8 62 :1994 . Conc re te t es t s –
Cons i s t ence o f f r esh l y m i xed conc re te , Pa r t 1 : S l ump
t es t s , Pa r t 2 : F l ow t es t , Pa r t 3 : Vebe t es t , Pa r t 4 :
Compac t i ng f ac to r and compac t i on i ndex . So u th A f r i can
Bu reau o f S tanda rds . P re to r i a .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
9-8
SANS 58 63 /SABS Me thod 863 -1994 . Conc re te t es t s –
Compres s i ve s t reng th o f ha rdened conc re te . 1 s t
Rev i s i on . Sou th A f r i can Bu reau o f S tanda rds . P re to r i a .
SANS 61 51 /SABS Me thod 863 -1994 . F reewa te r con ten t
o f Po r t l and cemen t ex tende rs . 1 s t Rev i s i on . Sou th
A f r i can Bu reau o f S tanda rds . P re to r i a .
SANS 61 56 /SABS Me thod 863 -1994 . Wa te r r equ i r emen t
o f Po r t l and cemen t ex tende rs . 1 s t Rev i s i on . Sou th
A f r i can Bu reau o f S tanda rds . P re to r i a .
SANS 6 157 /SABS Me tho d 863 -1994 . F i neness o f
cemen t and Po r t l and ceme n t ex ten de rs . 1 s t Rev i s i on .
Sou th A f r i can Bu reau o f S tanda rds . P re to r i a .
SANS 62 53 /SABS Me thod 863 -1994 . Conc re te t es t s –
Compres s i ve s t reng th o f ha rdened conc re te . 1 s t
Rev i s i on . Sou th A f r i can Bu reau o f S tanda rds . P re to r i a .
Schwar t z , K .P . 2 003 . The ou t l ook f o r CCPs . E lec t r i c
Pe rspec t i ves . Ju l y /Augus t 2003 .
S te f f an , P . and Dean , G . 19 91 . FGD Gypsum
U t i l i za t i on : Su rvey o f cu r ren t p rac t i ces and Assessmen t
o f Ma rke t Po ten t i a l . P roceed ings , A i r Was te
Managemen t Con fe rence . p . 1 .
Tang , F .J . and Ga r tne r , E .M . 1988 . I n f l uences o f
Su lpha te Sou rce on Po r t l and Cemen t Hyd ra t i on .
Advances i n Cemen t Resea rch . Vo lume 1 . Number 2 .
Ap r i l 1988 .
Tay lo r , H .F .W. 1982 . Cemen t Chem is t r y , 2 n d ed .
Te l f o rd . Rep r i n t ed 1982 .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
9-9
Uch i kawa , H . 1986 . E f f ec t o f b l end ing componen ts on
hyd ra t i on and s t r uc tu re f o rma t i on . P roceed ings , 8 t h
I n t e rna t i ona l Cong ress on t he Chem is t r y o f Cemen t s .
R io de Jane i r o , B raz i l . Sep t , 22 -27 . Spec ia l s Repo r t
Vo lume 1 .
Van Dyk , J .C . Keyse r , M . J . and Coe r t zen , M . 2005 .
Wor l d o f Coa l Ash Con fe rence . SASOL ’s un ique
pos i t i on i n SYNGAS P roduc t i on i n Sou th A f r i ca . Coa l
Sou rces us i ng SASOL Lu r g i F i xed Bed D r y Bo t t o m
Gas i f i e r s . Pape r P resen ted .
Wa inwr i gh t , P . J . and O lo runsogo , F .T . 1999 . E f f ec t s o f
PSD o f GGBS o n some du rab i l i t y p rope r t i es o f s l ag
cemen t mo r ta r s . Jou rna l o f t he Sou th A f r i can Ins t i t u t i on
o f C i v i l Eng inee r i ng . Vo lume 41 , Numb er 1 F i r s t
Qua r te r 1999 . pp 9 -17 .
Wa inwr i gh t , P . J . 2004 . Po r t l and Cemen t . Schoo l o f
C i v i l Eng inee r i ng . Un i ve r s i t y o f Leeds . Lec tu re r No tes .
www.wbc sdcemen t . o rg , agenda f o r sus ta i nab le
deve lopmen t . 2005 .
Yuan , R .L and Cook , J .E . 1983 . S tudy o f C lass C f l y
ash conc re te . F l y Ash , S i l i ca Fume , S lag and O the r
M ine ra l By -p rodu c t s i n Conc re te , f i r s t i n t e rna t i ona l
con fe rence . Mon tebe l l o , Canada . SP-79 . pp 307 -319 .
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
APPENDIX A
CUMULATIVE PARTICLE SIZE DISTRIBUTION OF GASIF ICATION
ASH, CEMENT AND GASIF ICATION ASH AND CEMENT
INTERGROUND AND INTERBLENDED
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
A-1
Cumulative Particle size distribution of Gasification ash
0
20
40
60
80
100
120
0.01 0.1 1 10 100 1000
Particle size (µm)
Cum
ulat
ive
part
icle
siz
e di
strib
utio
n % GA,30min
GA,1hr
GA,1.5hr
GA,2hrGA,2.5hr
GA,4hr
Cumulative Particle size distribution of Cement
0102030405060708090
100
0.01 0.1 1 10 100 1000
Particle size (µm)
Cum
ulat
ive
Part
icle
siz
e di
strib
utio
n %
CEM,30min
CEM,1hr
CEM,1.5hrCEM,2hr
CEM,2.5hr
CEM,4hr
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
A-2
Cumulative particle size distribution of gasification ash and cement interground
0102030405060708090
100
0.1 1 10 100 1000
Particle size (μm)
Cum
ulat
ive
part
icle
siz
e di
strib
utio
n %
IG, 30min
IG,1hr
IG,1.5hr
IG,2hr
IG,2.5hr
IG,4hr
Cumulative particle size distribution of gasification ash and cement interblended
0102030405060708090
100
0.1 1 10 100 1000
Particle size (μm)
Cum
ulat
ive
part
icle
siz
e di
strib
utio
n % IB 30 min
IB 1hrIB 1.5 hr
IB 2 hrIB 2.5hr
IB 4 hr
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
APPENDIX B
CUMULATIVE % OVERSIZE PARTICLE SIZE
DISTRIBUTIONS FOR GASIF ICATION ASH, CEMENT AND
GASIF ICATION ASH AND CEMENT INTERGROUND AND
INTERBLENDED
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
B-1
Cumulative % oversize particle size distribution
y = 0.9429e-0.0122x
R2 = 0.9991
0%
20%
40%
60%
80%
100%
0 50 100 150 200 250
Particle size (μm)
Cum
ulat
ive
% o
vers
ize
GA,30min
Expon. (GA,30min)
Cumulative % oversize particle size distribution
y = 0.9329e-0.0284x
R2 = 0.9989
0%
20%
40%
60%
80%
100%
0 20 40 60 80 100 120
Particle size (μm)
Cum
ulat
ive
% o
vers
ize
GA,1hr
Expon. (GA,1hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
B-2
Cumulative % oversize particle size distribution
y = 0.9331e-0.0382x
R2 = 0.9986
0%
20%
40%
60%
80%
100%
0 20 40 60 80
Particle size (μm)
Cum
ulat
ive
% o
vers
ize
GA,1.5hr
Expon. (GA,1.5hr)
Cumulative % oversize particle size distribution
y = 0.9452e-0.0507x
R2 = 0.9978
0%
20%
40%
60%
80%
100%
0 10 20 30 40 50 60
Particle size (μm)
Cum
ulat
ive
% o
vers
ize
GA,2hr
Expon. (GA,2hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
B-3
Cumulative % oversize particle size distribution
y = 0.9254e-0.0554x
R2 = 0.9981
0%
20%
40%
60%
80%
100%
0 10 20 30 40 50 60
Particle size (μm)
Cum
ulat
ive
% o
vers
ize
GA,2.5hrExpon. (GA,2.5hr)
Cumulative % oversize particle size distribution
y = 0.8942e-0.0781x
R2 = 0.9952
0%
20%
40%
60%
80%
100%
0 10 20 30 40
Particle size (μm)
Cum
ulat
ive
% o
vers
ize
GA,4hrExpon. (GA,4hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
B-4
Cumulative % oversize particle size distribution
y = 0.9675e-0.024x
R2 = 0.9936
0%
20%
40%
60%
80%
100%
0 50 100 150
Particle size (µm)
Cum
ulat
ive
% o
vers
ize
CEM,30min
Expon. (CEM,30min)
Cumulative % oversize particle size distribution
y = 0.7121e-0.0144x
R2 = 0.8842
0%
20%
40%
60%
80%
100%
0 50 100 150 200 250 300
Particle size (µm)
Cum
ulat
ive
% o
vers
ize
CEM,1hrExpon. (CEM,1hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
B-5
Cumulative % oversize particle size distribution
y = 0.9411e-0.0249x
R2 = 0.9858
0%
20%
40%
60%
80%
100%
0 50 100 150Particle size (µm)
Cum
ulat
ive
% o
vers
ize
CEM,1.5hr
Expon. (CEM,1.5hr)
Cumulative % oversize particle size distribution
y = 0.8794e-0.0237x
R2 = 0.9681
0%
20%
40%
60%
80%
100%
0 50 100 150 200
Particle size (µm)
Cum
ulat
ive
% o
vers
ize
CEM,2hr
Expon. (CEM,2hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
B-6
Cumulative % oversize particle size distribution
y = 0.9077e-0.0247x
R2 = 0.9791
0%
20%
40%
60%
80%
100%
0 50 100 150
Particle size (µm)
Cum
ulat
ive
% o
vers
ize
CEM,2.5hr
Expon. (CEM,2.5hr)
Cumulative % oversize particle size distribution
y = 0.8179e-0.0179x
R2 = 0.9454
0%
20%
40%
60%
80%
100%
0 50 100 150 200 250
Particle size (µm)
Cum
ulat
ive
% o
vers
ize
CEM,4hr
Expon. (CEM,4hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
B-7
Cumulative % oversize particle size distribution
y = 0.955e-0.0198x
R2 = 0.9996
0%
20%
40%
60%
80%
100%
0 50 100 150 200
Particle size (μm)
Cum
ulat
ive
% o
vers
ize
IG, 30min
Expon. (IG, 30min)
Cumulative % oversize particle size distribution
y = 0.975e-0.0354x
R2 = 0.9997
0%
20%
40%
60%
80%
100%
0 20 40 60 80 100
Particle size (μm)
Cum
alat
ive
% o
vers
ize
IG,1hr
Expon. (IG,1hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
B-8
Cumulative % oversize particle size distribution
y = 0.9929e-0.0514x
R2 = 0.998
0%
20%
40%
60%
80%
100%
0 20 40 60 80 100
Particle size (μm)
Cum
alat
ive
% o
vers
ize
IG,1.5hrExpon. (IG,1.5hr)
Cumulative % oversize particle size distribution
y = 0.9835e-0.05x
R2 = 0.9983
0%
20%
40%
60%
80%
100%
0 20 40 60 80 100
Particle size (μm)
Cum
alat
ive
% o
vers
ize
IG,2hr
Expon. (IG,2hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
B-9
Cumulative % oversize particle size distribution
y = 0.9693e-0.0532x
R2 = 0.9986
0%
20%
40%
60%
80%
100%
0 20 40 60 80 100
Particle size (μm)
Cum
alat
ive
% o
vers
ize
IG,2.5hr
Expon. (IG,2.5hr)
Cumulative % oversize particle size distribution
y = 0.9822e-0.0608x
R2 = 0.9963
0%
20%
40%
60%
80%
100%
0 20 40 60 80 100
Particle size (μm)
Cum
alat
ive
% o
vers
ize
IG,4hr
Expon. (IG,4hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
B-10
Cumulative % oversize particle size distribution
y = 0.9031e-0.0165x
R2 = 0.9874
0%
20%
40%
60%
80%
100%
0 50 100 150 200
Particle size (μm)
Cum
ulat
ive
% o
vers
ize
IB 30 min
Expon. (IB 30 min)
Cumulative % oversize particle size distribution
y = 0.8898e-0.023x
R2 = 0.9792
0%
20%
40%
60%
80%
100%
0 50 100 150 200
Particle size (μm)
Cum
ulat
ive
% o
vers
ize
IB 1hr
Expon. (IB 1hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
B-11
Cumulative % oversize particle size distribution
y = 0.9607e-0.03x
R2 = 0.9973
0%
20%
40%
60%
80%
100%
0 50 100 150 200
Particle size (μm)
Cum
ulat
ive
% o
vers
ize
IB 1.5 hrExpon. (IB 1.5 hr)
Cumulative % oversize particle size distribution
y = 0.945e-0.0334x
R2 = 0.9946
0%
20%
40%
60%
80%
100%
0 50 100 150 200
Particle size (μm)
Cum
ulat
ive
% o
vers
ize
IB 2 hr
Expon. (IB 2 hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
B-12
Cumulative % oversize particle size distribution
y = 0.9142e-0.0321x
R2 = 0.9897
0%
20%
40%
60%
80%
100%
0 50 100 150 200
Particle size (μm)
Cum
ulat
ive
% o
vers
ize
IB 2.5hr
Expon. (IB 2.5hr)
Cumulative % oversize particle size distribution
y = 0.8079e-0.0256x
R2 = 0.9545
0%
20%
40%
60%
80%
100%
0 50 100 150 200
Particle size (μm)
Cum
ulat
ive
% o
vers
ize
IB 4 hr
Expon. (IB 4 hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
APPENDIX C
ROSIN-RAMMLER DISTRIBUTION GRAPHS
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
C-1
Rosin-Rammler distribution graph
y = 0.9653x - 4.1996R2 = 1
0
0.5
1
1.5
0 2 4 6
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e %
ov
ersi
ze)
GA,30min
Linear (GA,30min)
Rosin-Rammler distribution graph
y = 0.958x - 3.347R2 = 1
0
0.5
1
1.5
0 1 2 3 4 5
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e %
ov
ersi
ze)
GA,1hr
Linear (GA,1hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
C-2
Rosin-Rammler distribution graph
y = 0.9589x - 3.0666R2 = 1
0
0.5
1
1.5
0 1 2 3 4 5
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e %
ov
ersi
ze)
GA,1.5hr
Linear (GA,1.5hr)
Rosin-Rammler distribution graph
y = 0.9665x - 2.8296R2 = 1
0
0.5
1
1.5
0 1 2 3 4 5ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e %
ov
ersi
ze)
GA,2hr
Linear (GA,2hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
C-3
Rosin-Rammler distribution graph
y = 0.9543x - 2.6897R2 = 1
0
0.5
1
1.5
0 1 2 3 4 5
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e %
ov
ersi
ze)
GA,2.5hrLinear (GA,2.5hr)
Rosin-Rammler distribution graph
y = 0.934x - 2.2793R2 = 0.9999
0
0.5
1
1.5
0 1 2 3 4
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e %
ov
ersi
ze)
GA,4hr
Linear (GA,4hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
C-4
Rosin-Rammler distribution graph
y = 0.9816x - 3.6309R2 = 1
0
0.5
1
1.5
0 2 4 6 8
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e %
ov
ersi
ze)
CEM,30min
Linear (CEM,30min)
Rosin-Rammler distribution graph
y = 0.816x - 3.1629R2 = 0.9984
0
0.5
1
1.5
0 1 2 3 4 5 6
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e %
ov
ersi
ze)
CEM,1hr
Linear (CEM,1hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
C-5
Rosin-Rammler distribution graph
y = 0.9662x - 3.5129R2 = 1
0
0.5
1
1.5
0 1 2 3 4 5 6
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e %
ov
ersi
ze)
CEM,1.5hrLinear (CEM,1.5hr)
Rosin-Rammler distribution graph
y = 0.9307x - 3.3684R2 = 0.9999
0
0.5
1
1.5
0 2 4 6
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e %
ov
ersi
ze)
CEM,2hr
Linear (CEM,2hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
C-6
Rosin-Rammler distribution graph
y = 0.9469x - 3.4172R2 = 0.9999
0
0.5
1
1.5
0 2 4 6
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e %
ov
ersi
ze)
CEM,2.5hr
Linear (CEM,2.5hr)
Rosin-Rammler distribution graph
y = 0.8908x - 3.4053R2 = 0.9996
0
0.5
1
1.5
0 1 2 3 4 5 6
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e %
ov
ersi
ze)
CEM,4hrLinear (CEM,4hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
C-7
Rosin-Rammler distribution graph
y = 0.9743x - 3.7795R2 = 1
0
0.5
1
1.5
0 1 2 3 4 5 6
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e pa
rtic
le
size
dis
trib
utio
n)
IG, 30min
Linear (IG, 30min)
Rosin-Rammler distribution graph
y = 0.9848x - 3.2664R2 = 1
0
0.5
1
1.5
0 1 2 3 4 5
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e pa
rtic
le
size
dis
trib
utio
n)
IG,1hr
Linear (IG,1hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
C-8
Rosin-Rammler distribution graph
y = 0.9959x - 2.9494R2 = 1
0
0.5
1
1.5
0 1 2 3 4 5
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e pa
rtic
le
size
dis
trib
utio
n)
IG,1.5hr
Linear (IG,1.5hr)
Rosin-Rammler distribution graph
y = 0.9902x - 2.951R2 = 1
0
0.5
1
1.5
0 1 2 3 4 5
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e pa
rtic
le
size
dis
trib
utio
n)
IG,2hr
Linear (IG,2hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
C-9
Rosin-Rammler distribution graph
y = 0.9813x - 2.8498R2 = 1
0
0.5
1
1.5
0 1 2 3 4 5
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e pa
rtic
le
size
dis
trib
utio
n)
IG,2.5hr
Linear (IG,2.5hr)
Rosin-Rammler distribution graph
y = 0.9896x - 2.7544R2 = 1
0
0.5
1
1.5
0 1 2 3 4 5
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e pa
rtic
le
size
dis
trib
utio
n)
IG,4hr
Linear (IG,4hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
C-10
Rosin-Rammler Distribution graph
y = 0.9424x - 3.7753R2 = 0.9999
0
0.5
1
1.5
0 2 4 6
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e pa
rtic
le
size
dis
trib
utio
n)
IB 30 min
Linear (IB 30 min)
Rosin-Rammler Distribution graph
y = 0.9348x - 3.4207R2 = 0.9999
0
0.5
1
1.5
0 2 4 6
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e pa
rtic
le
size
dis
trib
utio
n)
IB 1hrLinear (IB 1hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
C-11
Rosin-Rammler Distribution graph
y = 0.9777x - 3.3921R2 = 1
0
0.5
1
1.5
0 2 4 6
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e pa
rtic
le
size
dis
trib
utio
n)
IB 1.5 hr
Linear (IB 1.5 hr)
Rosin-Rammler Distribution graph
y = 0.9686x - 3.2527R2 = 1
0
0.5
1
1.5
0 2 4 6
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e pa
rtic
le
size
dis
trib
utio
n)
IB 2 hrLinear (IB 2 hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
C-12
Rosin-Rammler Distribution graph
y = 0.9499x - 2.0479R2 = 0.9999
0
0.5
1
1.5
0 2 4
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e pa
rtic
le
size
dis
trib
utio
n)
IB 2.5hr
Linear (IB 2.5hr)
Rosin-Rammler Distribution graph
y = 0.8839x - 3.0507R2 = 0.9995
0
0.5
1
1.5
0 2 4 6
ln (Particle size(µm))
ln ln
(1/C
umul
ativ
e pa
rtic
le
size
dis
trib
utio
n)
IB 4 hr
Linear (IB 4 hr)
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
APPENDIX D
BLAINE SURFACE AREA CALCULATIONS
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
D-1
Cement 7.83gr RD = 3.2 Sample time (sec) cm2/g m2/g
30 min 125.1 3147 3151 hour 138.9 3316 3321.5 hours 175.3 3726 3732 hours 217.1 4146 4152.5 hours 228.5 4254 4254 hours 227.6 4245 425 Gasification ash 6.65gr RD =2.715
Sample time (sec) cm2/g m2/g 30 min 68 2320 2321 hour 173.8 3710 3711.5 hours 253.8 4483 4482 hours 355 5302 5302.5 hours 437.7 5887 5894 hours 668.5 7275 728 Intergrinding 7.28gr RD = 2.976
Sample time (sec) cm2/g m2/g 30 min 131.4 3226 3231 hour 186.2 3840 3841.5 hours 255.4 4497 4502 hours 333 5135 5132.5 hours 348 5249 5254 hours 558.1 6648 665
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
APPENDIX E
MORTAR PRIS MS STREN G TH SU MMAR Y FOR THE E FFECT OF GRINDING T IME ON THE PROPERTIES OF INTERBL ENDE D
GASIF I C AT ION A SH AN D CEMENT
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
E-1
Summary Table
Interblending Gasification ash and Cement
Compression (MPa)
30 min
1 hour
1.5 hours 2 hours 2.5
hours 4
hours Cement (2 hrs)
2 days 10.1 11.9 11.2 20.1 18.4 17.6 17.6
7 days 19.5 24.1 23.5 34.3 29.7 31.3 31.5
28 days 30.8 32.1 33.1 45.1 45.4 43 44.9
Tension (MPa) 30 min
1 hour
1.5 hours 2 hours 2.5
hours 4
hours Cement
(2 hours)
2 days 3 3.5 3.3 4.9 4.5 4.8 3.8
7 days 5.2 5.8 5.5 7.3 6.7 7.4 7.3
28 days 7.3 7.7 8.2 8.9 8.8 8.9 8.2
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
APPENDIX F
MORTAR PRIS MS STREN G TH SU MMAR Y FOR THE E FFECT OF GRIN DIN G T IME ON TH E PROPERTIES OF INTERGROUND
GASIF I C AT ION A SH AN D CEMENT
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
F-1
Summary Table
Intergrinding Gasification Ash and Cement
Compression (MPa)
30 min 1 hour 1.5
hours 2
hours 2.5
hours 4 hours Cement (2 hours)
2 days 11.8 13.3 17 21.5 19.5 19.2 17.6
7 days 19.4 24.6 29.3 32.4 31.6 31.7 31.5
28 days 27.3 32.9 40.1 43.2 41.6 43.6 44.9
Tension (MPa) 30 min 1 hour 1.5
hours 2
hours 2.5
hours 4 hours Cement (2 hours)
2 days 3 3.4 4.2 4.8 4.5 5.1 3.8
7 days 4.6 6 6.5 7.3 6.7 7.2 7.3
28 days 7 8 8.8 8.6 9 8.8 8.2
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
APPENDIX G
MORTAR PRIS MS STREN G TH SU MMAR Y FOR THE EFFECT OF GYPSUM CONT ENT ON THE PROPE RTIES OF INTERGROUND
GASIF I C AT ION A SH AN D CEMENT
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
G-1
Summary Table
Gypsum Content
Compression (MPa) 0% 0.50% 1% 1.50% 2% 2.50% 3%
2 days 10.7 11.1 11.7 11.6 12 12.1 15.2
7 days 25.1 24.5 24.9 25.7 27.6 25.7 28.6
28 days 33.7 36.1 36.9 32.9 36.2 37.1 38.9
Tension (MPa) 0% 0.50% 1% 1.50% 2% 2.50% 3%
2 days 3.2 3.3 3.2 3.4 3.3 3.3 4.5
7 days 6 6 5.5 6.2 5.9 5.7 6.2
28 days 7.0 7.8 7.7 7.5 8.0 7.7 7.6
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
APPENDIX H
MORTAR PRIS MS STREN G TH SU MA RY FOR THE EFF ECT OF REPLACEME NT L EVEL ON THE PROPE RTIE S OF
INTER GR OUN D GASIF ICA T ION A S H AND C EME NT
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
H-1
Summary Table
Replacement Level
Compression (MPa) 0% 10% 20% 35% 55%
2 Days 32.1 34.4 26.1 18.3 6.5
7 Days 47.0 50.3 45.4 32.6 16.9
28 Days 56.9 57.9 53.2 43.3 28.9
Tension (MPa) 0% 10% 20% 35% 55%
2 Days 6.8 7.2 4.7 4.3 1.5
7 Days 8.8 9.2 9.1 7.2 4.4
28 Days 9.7 9.8 9.6 9.5 7.5
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
APPENDIX I
MORTAR PRIS MS STREN G TH SU MMAR Y FOR THE C OMPARI SON BETWEE N MA NUF ACTU RE D AND C OMME RC IAL CE MENT
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
I-1
Summary Table
Compression (MPa) IB CEM+GYPSUM IG CEM +GYPSUM CEM I 42.5 R
2 Days 18.8 29.8 22.3
7 Days 34.5 49.4 36.2
28 Days 42.0 61.5 53.0
Tension (MPa) IB CEM+GYPSUM IG CEM +GYPSUM CEM I 42.5
2 Days 4.2 5.9 5.0
7 Days 6.4 8.3 7.8
28 Days 8.3 10.0 9.9
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
APPENDIX J
CUBE ST REN GTH SUMMA R Y
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
J-1
Cube St rength Summary Table
Summary 24 hour 7 days 28 days
IG (MPa) 6.33 22.64 31.5
IB FA (MPa) 6.31 15.93 26.7
IB GA (MPa) 7.59 19.29 28.0
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
APPENDIX K
SPECIF I C CRE EP SUMMARY
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
K-1
Speci f ic Creep Summary Table
T ime (days) IG GA (microst ra in )
IB FA (microst ra in )
IB GA (microst ra in )
0 0 .00 0 .00 0 .00
1 10 .48 4 .15 11 .13
2 14 .30 20 .25 21 .80
3 24 .30 29 .59 30 .61
7 38 .12 44 .65 42 .67
8 43 .84 51 .92 48 .70
10 49 .08 57 .63 53 .80
13 58 .61 68 .02 64 .47
15 67 .19 77 .88 72 .82
17 71 .48 83 .59 75 .60
41 97 .69 97 .09 89 .98
48 116 .27 113 .70 115 .49
53 120 .08 120 .97 116 .42
64 129 .61 124 .09 119 .20
120 148 .20 137 .07 136 .83
127 155 .82 142 .78 141 .00
132 159 .16 145 .89 143 .78
146 163 .92 153 .68 150 .28
167 171 .07 160 .95 158 .16
269 188 .23 175 .49 173 .00
309 201 .09 169 .78 184 .60
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
APPENDIX L
POROSIT Y SUMMARY
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
L-1
Summary Table
M ix Poros i ty
IG 15 .1%
IB FA 15 .9%
IB GA 15 .4%
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
APPENDIX M
PERMEABIL ITY CALCUL ATIONS
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))
M-1
Summary Table
M ix IG IB FA IB GA Pressure bar 2 2 2 2 2 2 2 2 2
Diamete r (m) 0 .06935 0 .0694 0 .06935 0 .0693 0 .0694 0 .06935 0 .0694 0 .0694
5 0 .0693
5
Area (m 2 ) 0 .003777312
0 .00378276
0 .0037773
0 .003771867
0 .003783
0 .003777
0 .00378276
0 .003788
0 .003777
T ime average ( s ) 4 .85 10 .93 8 .29 12 .83 10 .81 11 .15 11 .53 8 .29 9 .79
Read ing ( m 3 /s ) 1 .88262E-05
8 .3735E-06 1 .1E -05 7 .10137E-
06 8 .42E-
06 7 .78E-
06 7 .85095E
-06 1 .08E-
05 9 .38E-
06 Th ickness o f
d isc (m) 0 .02 0 .02 0 .02 0 .02 0 .02 0 .02 0 .02 0 .02 0 .02
e 2 .02E-16 2 .02E-16 2 .02E-16 2 .02E-16 2 .02E-
16 2 .02E-
16 2 .02E-16 2 .02E-16
2 .02E-16
Permeab i l i t y (m /s ) 1 .621E-20 7 .213E-
21 9 .461E-
21 6 .125E-21 7 .21E-21
6 .37E-21
6 .688E-21
9 .07E-21
8 .14E-21
Permeab i l t y average (m /s ) 1 .096E-20 6 .569E-21 7 . 967E-21
OPI 19 .96 20 .18 20 .098
UUnniivveerrssiittyy ooff PPrreettoorriiaa eettdd –– DDuu PPlleessssiiss HH ((22000066))