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© Sara Hallin
Biological N and P removal in activated sludge processes
Sara Hallin Department of Microbiology, SLU
Metabolism
Oxidation:
KOLFÖRENING KOLDIOXID + ELEKTRONER + VÄTEJONER
Reduktion:
SYRE + ELEKTRONER + VÄTEJONER VATTEN
Fullständig reaktion:
KOLFÖRENING + SYRE KOLDIOXID + VATTEN
BIOKEMISKT BUNDEN ENERGI
Fermentation:
GLUKOS ETANOL + KOLDIOXID
BIOKEMISKT BUNDEN ENERGI
Fermentation av socker till etanol och koldioxid. En del av kolet isockret har oxiderats till koldioxid medan en del har reducerats tilletanol (vanlig sprit).
Organiskt material bryts ner av mikroorganismer i luftningsbassängen. Slammet (biomassa och organiskt material)avskiljs från det renade vattnet i sedimenteringsbassängen. .
Traditionell ASP
NH4+ NO2
- NO3-
N2O NO NO2
-
Organically bound nitrogen org-NH2
N2
Nitrogen fixation
Nitrification
Assimilation
Assimilation Mineralization/ Ammonification
ATMOSPHERE
SOIL/WATER
Denitrification
Dissimilatory nitrate reduction to ammonium
Microbiological reactions in the N cycle
Nitrification in water treatment
Nitrification lowers BOD load in recipient Nitrification coupled to denitrification lowers N load in recipient Nitrogen removal systems: - natural wetlands - constructed wetlands - wastewater treatment plants Process problems with inhibition: Microbial sensors for detecting nitrification inhibitors
Nitrification
Nitrosomonas
Nitrification involves several reactions and two different bacteria: 1. Dissociation of ammonium 2. Oxidation of ammonia Ammonia monooxygenase (AMO): Integral membrane protein Can oxidize methane Cometabolize halogenated compounds 3. Oxidation of hydroxylamine Hydroxylamine oxidoreductase (HAO): Soluble, periplasmic protein 4. Oxidation of nitrite
Ammonia oxidation: NH3 + 1,5O2 NO2
- + H+ + H2O
Periplams
OH-
Nitrite oxidation: NO2- + ½ O2 NO3
-
Carbon metabolism
Cell constituents Growth
Energetic constraints...
1. ATP and NADPH (reducing power) requirements in Calvin cycle
2. NAD(P)H formed by reverse e- flow:
Cyt c 2e- Cyt c
O2
NAD(P)+ e-
e-
Am
mo
nia
oxi
diz
ing
arc
ha
ea
an
d
ba
cte
ria
(A
OA
an
d A
OB
) The organisms
NH3 oxidizers Proteobacteria: Nitrosomonas Nitrosococcus Nitrosospira Thaumarchaeota: Nitrosopumilis…
NO2- oxidizers
Bacteria: Nitrobacter Nitrospira
NH4+ NO2
- NO3-
N2O NO NO2
-
Organically bound nitrogen org-NH2
N2
Nitrogen fixation
Nitrification
Assimilation
Assimilation Mineralization/ Ammonification
ATMOSPHERE
SOIL/WATER
Denitrification
Dissimilatory nitrate reduction to ammonium
Microbiological reactions in the N cycle
Denitrifikation är en andningsprocess som där nitrat omvandlas till kvävgas i flera komplicerade steg inom en och samma bakteriecell:
nitrat → nitrit → kväveoxid → lustgas → kvävgas
(NO3- → NO2
- → NO → N2O → N2)
Denitrification Pathway
O2 + = NO3
-/ NO2
-
Denitrification pathway
Denitrification: anaerobic respiration
Organic compound CO2
Biosynthesis
Carbon flow
NO3-, (NO2
-, N2O)
Electron flow ATP
Denitrification
Cytoplasma
Periplasma
NO3-
NO2- NO3
-
H+
NADH2 NAD+
Proton motive force
2e- 2e- 2e-
NO2- NO
NO N2O
N2O N2
e- nar nor
nir nos
Denitrifier Diversity
Denitrifiers
Bacteria Eukarya Archaea
Denitrifier diversity
O2
NH4+
H20 O2
ATP
Nitrifikation
NO2-
Redox
+
Glucose
2 ATP 2 NADH Glykolysis
2 Pyruvate
2 GTP
6 CO2
TCA cycle 8 NADH
2 FADH
ATP NADH
FADH ATP
NO3- NO2
- NO N2O N2
- Denitrifikation
NO 2 NO N 2 O N 2 NO 2 NO N 2 O N 2 NO 3 NH 4 NH 2 OH NO 2 NO - 3 NH NH 2 OH NO 2 - - +
Kvävrening
Nitrifierande bakterier Denitrifierande bakterier •Nitrifierare finns i mark och vatten •Bara några få arter •Nitrifikation är två energigivande processer som utförs av två olika grupper av bakterier •Nitrifierare växer långsamt
•Denitrifierare finns nästan överallt •Många bakteriesläkten •Denitrifikation är en alternativ andningsprocess i frånvaro av syre •Denitrifierare är växer oftast snabbt
Effekt av extern kolkälla på kvävereningen
0
20
40
60
80
100
0 10 20 30 40 50 60
R
E
0
5
10
15
0 10 20 30 40 50 60
R
E
1. Kvävereningsgrad (%): 2. Denitrifikastionskapacitet:
Tid (dagar) Tid (dagar)
R = Fördenitrifikation utan extern kolkälla E = Fördenitrifikation med etanoltillsats
Intermittent dosering av etanol i en fördenitrifikationsprocess
Hasselblad & Hallin. 1998. Wat. Sci.Technol.
NO 2 NO N 2 O N 2 NO 2 NO N 2 O N 2 NO 3 NH 4 NH 2 OH NO 2 NO - 3 NH NH 2 OH NO 2 - - +
Kvävrening
D I E T A G R I C U L T U R E E N V I R O N M E N T
1/3 of denitrifier genomes lack nosZ (Jones et al. 2008 Molec Biol Evol)
0
0,2
0,4
0,6
0,8
Ratio of N2O-producers
N2O
/(N
2O+
N2)
Manipulation of soil denitrifier community showed direct causality link between the community composition and potential N2O emissions. (Philippot et al. 2011 Global Change Biol.)
Some organisms only have nosZ and are potential N2O sinks. (Graf et al. in prep.)
Microber med och utan nosZ (N2O reduktase gen)
World greenhouse gas emissions by sector
Biological phosphorus removal
ANAEROBIC AEROBIC
Energy Phosphate
Short chain fatty acids
Energy Phosphate O2
CO2+H2O
Energy consumption for uptake of soluble organics. ATP and PO43- is released.
Energy is conserved as poly- phosphate granules. Uptake of PO4
3-. Consumption of stored products (PHB).
PHB synthesis & degradation
Acetoacetate ß-hyroxybutyryl-CoA
ß-hydroxybutyrate
Acetoacetyl-CoA
Poly-ß-hyroxybutyrate (PHB)
Acetic acid Acetyl-CoA
Biological phosphorus removal
PO43- O2
CO2+H2O Energy Energy PO4
3- Organics
Den
itri
fica
tion
ANAEROBIC REACTOR AEROBIC REACTOR SEDIMENTATION
Recirculation of NO3-
N-removal in wetlands
CH4 O2
Diffusion through aerenchyma
Water
O2
CO2
CO2 CH4
O2 +NH3 NO3-
N2OO2
CH4
H2+CO2
Acetate
Root exudates
N2
CO2Reduction zone
NO3- Aerobic zoneN2O N2
Anaerobic zone
NO3-
Reduction zoneSO4
2-
Reduction zone
NO3-
O2
O2 + NH3
CH4 O2
Diffusion through aerenchyma
Water
O2
CO2
CO2 CH4
O2 +NH3 NO3-
N2OO2
CH4
H2+CO2
Acetate
Root exudates
N2
CO2Reduction zone
NO3- Aerobic zoneN2O N2
Anaerobic zone
NO3-
Reduction zoneSO4
2-
Reduction zone
NO3-
O2
O2 + NH3
Constructed wetlands
µg
N/g
DW
/h
Ruiz et al., 2009, FEMS Microbiol. Ecol.
Plants affect denitrification
We
tla
nd
pla
nts
eff
ec
ts
Rhiz
ospe
here
Se
dim
ent
Low rates
High rates
Ruiz et al., 2009, FEMS Microbiol. Ecol.
DGGE of nosZ
• Typha and Fragmites select nosZ communities • Seasonal differences
• Typha and Phragmites select nosZ communities • Typha and Phragmites increase denitrification activity • Seasonal differences Is increase in rhizosphere enough for increased capacity of wetland? • What about the abundance of denitrifiers?
Conclusions and outlook
Ekeby Constructed Wetland
Ekeby wetland in Eskilstuna
Total area: 36 ha
Flow: ~45000m3/day
Wat
er-
flo
w p
ath
s
Kjellin et al., 2007, Wat. Res.
11.113.04103.2 NR CTPDA −−×=Multiple regressions: D
en
itri
fic
atio
n r
ate
s
Kjellin et al., 2007, Wat. Res.
N-removal in mining impacted waters