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1 Compressibility of Soil Chih Chih- Ping Lin Ping Lin National National Chiao Chiao Tung Tung Univ. Univ. [email protected] [email protected] Soil Mechanics 2 Outline Introduction Introduction Immediate Settlement Immediate Settlement Primary Consolidation Settlement Primary Consolidation Settlement Consolidation Settlement Consolidation Settlement Consolidation Rate Consolidation Rate Secondary Consolidation Settlement Secondary Consolidation Settlement

Soil Mechanics − Outline

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Page 1: Soil Mechanics − Outline

1

Compressibility of Soil

ChihChih--Ping LinPing LinNational National ChiaoChiao TungTung [email protected]@mail.nctu.edu.tw

Soil Mechanics −

2

Outline

IntroductionIntroduction

Immediate SettlementImmediate Settlement

Primary Consolidation SettlementPrimary Consolidation SettlementConsolidation SettlementConsolidation Settlement

Consolidation RateConsolidation Rate

Secondary Consolidation SettlementSecondary Consolidation Settlement

Page 2: Soil Mechanics − Outline

3

δ versus δD

(a)Leaning Tower, Pisa

(b) Palacio de las BellasArtes, Mexico City

(The Palace of Fine Arts)

Introduction

4

Types of Settlements

Immediate (elastic) settlement (Immediate (elastic) settlement (SSee))

TimeTime--dependentdependentPrimary consolidation (Primary consolidation (SScc) ) transient pore transient pore pressurepressure

Secondary consolidation (Secondary consolidation (SSss) ) creepcreep

Total settlement STotal settlement STT==SScc+S+Sss+S+See

For soft soils (i.e., clays): SFor soft soils (i.e., clays): Scc>>S>>See>S>Ss s (Usually)(Usually)

Introduction

Page 3: Soil Mechanics − Outline

5

Contact Pressure and Settlement Profile

Immediate Settlement

Clay Sand

6

Theory of Elasticity

Immediate Settlement

Δσ

Es,μs

B

ps

se I

EBS

21 μσ

−Δ=

Influence Factor

(shape, position, foundation rigidity)

Page 4: Soil Mechanics − Outline

7

Improved Relationship for Se

EFGs

ee IIIE

BS0

21 μσ

−Δ= Foundation embedment

Foundation rigidity

Equivalent diameter

Immediate Settlement

8

©20

01 B

rook

s/C

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ivis

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of T

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son

Lea

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nc.

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earn

ing ™

is a

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erei

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der

licen

se.

Immediate Settlement

Page 5: Soil Mechanics − Outline

9

©20

01 B

rook

s/C

ole,

a d

ivis

ion

of T

hom

son

Lea

rnin

g, I

nc.

Tho

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n L

earn

ing ™

is a

trad

emar

k us

ed h

erei

n un

der

licen

se.

Immediate Settlement

10

©20

01 B

rook

s/C

ole,

a d

ivis

ion

of T

hom

son

Lea

rnin

g, I

nc.

Tho

mso

n L

earn

ing ™

is a

trad

emar

k us

ed h

erei

n un

der

licen

se.

Immediate Settlement

Page 6: Soil Mechanics − Outline

11

Fundamentals of ConsolidationConsolidation Settlement

Δu =Δσ

Δσ’=0

Δu =0

Δσ’= Δσ

12

Consolidation Settlement

Page 7: Soil Mechanics − Outline

13

Consolidation Settlement

14

What is Consolidation?

When a saturated clay is loaded externally,

saturated clay

GL

the water is squeezed out of the clay over a long time (due to low permeability of the clay).

Consolidation Settlement

Page 8: Soil Mechanics − Outline

15

What is Consolidation?

This leads to settlements occurring over a long time,

which could be several years.

time

sett

lem

ent

Consolidation Settlement

16

In granular soils…

Granular soils are freely drained, and thus the settlement is instantaneous.

time

sett

lem

ent

Consolidation Settlement

Page 9: Soil Mechanics − Outline

17

During consolidation…

Due to a surcharge q applied at the GL,

GL

saturated clay

q kPa

A

the stresses and pore pressures are increased at A.

Δσ

Δu

Δσ’

..and, they vary with time.

Consolidation Settlement

18

During consolidation…

Δσ remains the same (=q) during consolidation.

GL

saturated clay

q kPa

A

Δσ

Δu

Δσ’

Δu decreases (due to drainage)

Δσ

Δu

Δσ’

q

transferring the load from water to the soil.while Δσ’ increases,

Consolidation Settlement

Page 10: Soil Mechanics − Outline

19

One Dimensional Consolidation

~ drainage and deformations are vertical (none laterally)

saturated clay

GL

q kPa

~ a simplification for solving consolidation problems

reasonable simplification if the

surcharge is of large lateral extent

water squeezed out

Consolidation Settlement

20

ΔH -Δe Relation

saturated clay

GL

q kPa

Ho

Time = 0+

e = eo

ΔH

saturated clay

GL

q kPa

Time = ∝

e = eo - Δe

average vertical strain = oH

Consolidation Settlement

Page 11: Soil Mechanics − Outline

21

ΔH -Δe Relation

Consider an element where Vs = 1 initially.

Δe

1

eo

Time = 0+ Time = ∞

∴average vertical strain =oe

e

1

Consolidation Settlement

22

ΔH -Δe Relation

Equating the two expressions for average vertical strain,

oe

e

1=

Δ

oH

H

consolidation settlement

initial thickness of clay layer

initial void ratio

change in void ratio

Consolidation Settlement

Page 12: Soil Mechanics − Outline

23

Coefficient of volume compressibility

~ denoted by mv

~ is the volumetric strain in a clay element per unit increase in stress

volumeoriginal

volumein change=

σΔ

Δ= V

Vmv

i.e.,

no units

kPa or MPakPa-1 or MPa-1

Consolidation Settlement

Coefficient of compressibility

~ denoted by av = Δe/Δσ

24

Consolidation Test

~ simulation of 1-D field consolidation in lab.

field

GL

lab

undisturbed soil specimen

Dia = 50-75 mm

Height = 20-30 mm

metal ring(oedometer)

porous stone

Consolidation Settlement

Page 13: Soil Mechanics − Outline

25

Consolidation Test

ΔH1

Δq1

eo- Δe1

)1(11 o

o

eH

He +

Δ=Δ

eoHo

Δq2

loading in increments

=Δ 2e

allowing full consolidation before next increment

Consolidation Settlement

26

Consolidation Test

unloading

Consolidation Settlement

Page 14: Soil Mechanics − Outline

27

e – log σv’ plot

log σv’

void

rat

io loading

σv’ increases &

e decreasesunloading

σv’ decreases &

e increases (swelling)

- from the above data

Consolidation Settlement

28

Compression and recompression indices

log σv’

void

rat

io

1

Cc

Cc ~ compression index

Cr ~ recompression index(or swelling index)

1Cr

1Cr

Consolidation Settlement

Page 15: Soil Mechanics − Outline

Preconsolidation pressure

log σv’

void

rat

io

σp’preconsolidation pressure

is the maximum vertical effective stress the soil

element has everbeen subjected

to

Consolidation Settlement

30

Virgin Consolidation Line

log σv’

void

rat

io

virgin consolidation line

σp’σvo’

eo

eo, σvo’

original state

Consolidation Settlement

Page 16: Soil Mechanics − Outline

Overconsolidation ratio (OCR)

log σv’

void

rat

io

virgin consolidation line

σp’σvo’

eo

original state

Field

σvo’

'

'

vo

pOCRσσ

=

Consolidation Settlement

32

Consolidation Settlement

δ-logt or e-logt plot for each loading step

Page 17: Soil Mechanics − Outline

33

e-logσ’ plot for all loading steps

Consolidation Settlement

34

Determining Cc, Cr, Preconsolidation Pressure

Casagrande’s Method

Consolidation Settlement

Page 18: Soil Mechanics − Outline

35

Effect of Disturbance

Normally consolidatedClay of low to mediumplasticity

Consolidation Settlement

36

Effect of Disturbance

Over-consolidatedClay of low to mediumplasticity

Consolidation Settlement

Page 19: Soil Mechanics − Outline

37

Calculating Consolidation Settlement

Consolidation Settlement

Settlement computations

eo, σvo’, Cc, Cr, σp’, mv-oedometer

test

Δσ=q

q kPa

H

Two different ways to estimate the consolidation settlement:

(a) using mv

(b) using e-log σv’ plot

settlement = mv Δσ H

He

esettlement

o+Δ

=1

next slide

Consolidation Settlement

Page 20: Soil Mechanics − Outline

Settlement computations

~ computing Δe using e-log σv’ plot

'

''log

vo

vocCe

σσσ Δ+

initial

σvo’

eo

σvo’+ Δσ

Δe

If the clay is normally consolidated,

the entire loading path is along the VCL.

Consolidation Settlement

Settlement computations

~ computing Δe using e-log σv’ plot

'

''log

vo

vorCe

σσσ Δ+

σvo’

initialeo

σvo’+ Δσ

If the clay is overconsolidated, and remains so by the end of consolidation,

Δe

VCL

note the use of Cr

Consolidation Settlement

Page 21: Soil Mechanics − Outline

Settlement computations

~ computing Δe using e-log σv’ plot

'

''log

'

'log

p

voc

vo

pr CCe

σσσ

σσ Δ+

+=Δ

σvo’

initialeo

σvo’+ Δσ

If an overconsolidated clay becomes normally consolidated by the end of consolidation,

VCL

σp’

Δe

Consolidation Settlement

42

Calculation of Consolidation Settlement under a Foudation

Consolidation Settlement

Page 22: Soil Mechanics − Outline

43

More to come…

44

Time Rate of Consolidation

Consolidation Rate

Page 23: Soil Mechanics − Outline

45

Governing Eqn

Consolidation Rate

46

Consolidation Rate

Page 24: Soil Mechanics − Outline

47

Solution of Consolidation Equation

Consolidation Rate

48

Consolidation Rate

Page 25: Soil Mechanics − Outline

49

Consolidation Rate

50

Consolidation Rate

Page 26: Soil Mechanics − Outline

51

Consolidation Rate

52

Determining Cv (logarithmic method)

Consolidation Rate

Page 27: Soil Mechanics − Outline

53

Determining Cv (square root method)

Consolidation Rate

54

Secondary consolidation

Secondary Consolidation Settlement

Page 28: Soil Mechanics − Outline

55