Estimation of CH4 and N2 O emissions from rice fields under AWD irrigation management through a DNDC model approachEstimation of CH4 and N2 O emissions from rice fields under AWD irrigation management through a DNDC model approach
Estimation of CH4 and N2 O emissions from rice fields under
AWD irrigation management through a DNDC model approach
Managing Climate Change (MC2)
“Process, Measurements, Modelling and Mitigation of Greenhouse Gasses” 18-20 November 2009
Massey University, Palmerston North, New Zealand Managing Climate Change (MC2)
“Process, Measurements, Modelling and Mitigation of Greenhouse Gasses” 18-20 November 2009
Massey University, Palmerston North, New Zealand
N. Katayanagi1,2, Y. Furukawa2,3, T. Fumoto4, and Y. Hosen1,2
1 Japan International Research Center for Agricultural Sciences,Tsukuba, Japan 2 International Rice Research Institute, Los Baños, Philippines
3 Niigata Agricultural Research Institute, Nagaoka, Japan (present address)
N. Katayanagi1,2, Y. Furukawa2,3, T. Fumoto4, and Y. Hosen1,2
1 Japan International Research Center for Agricultural Sciences, Tsukuba, Japan 2 International Rice Research Institute, Los Baños, Philippines
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Table of Contents
Table of Contents
1. Background
2. Modification of DNDC-Rice model
3. Model Validation
4. Summary
1.
Background
2.
Modification of DNDC-Rice model
3.
Model Validation
Table of Contents
Table of Contents
1. Background
2. Modification of DNDC-Rice model
3. Model Validation
4. Summary
1.
Background
2.
Modification of DNDC-Rice model
3.
Model Validation
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4
Alternate Wetting and Drying
A
lternate
W
etting and
D
rying
A Water-saving irrigation technique for rice cropping AWD has been investigated by International Rice
Research Institute (IRRI) in Philippines since the early 1970’s.
With the technique:
• 15-30% unproductive water outflow can be cut down • Water productivity can be increased without
sacrificing yield.
The main objectives of research for AWD technique are: • The spread of the technique
• The evaluation of the technique from the viewpoint of its environmental impact
A Water-saving irrigation technique for rice cropping
AWD has been investigated by International Rice
Research Institute (IRRI) in Philippines since the early 1970’s.
With the technique:
• 15-30% unproductive water outflow can be cut down
• Water productivity can be increased without
sacrificing yield.
The main objectives of research for AWD technique are:
• The spread of the technique
• The evaluation of the technique from the viewpoint of
its environmental impact
Criteria of driest conditions,
e.g. Certain soil water tension at 150 mm depth or
Criteria of driest conditions,
e.g. Certain soil water tension at 150 mm depth or Maximum height of standing water, e.g. + 50mm Continuously flooding Continuously flooding
AWD
AWD
Soil Soil Time Standing waterIrrigation Timing of AWD technique
Irrigation Timing of AWD technique
AWD
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Field water tube
Instruments for monitoring hydrological conditions
Instruments for monitoring hydrological conditions
Tensiometer
AWD
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GHGs measurement conducted in IRRI since 2007
GHGs measurement conducted in IRRI since 2007
AWD
AWD
Irrigation Water Plenty
Global warming potential
High 0
CH
4CH
4N
2O
N
2O
Total
GWP
Total
GWP
AWD can decrease GWP of paddy fields
AWD can decrease GWP of paddy fields
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Table of Contents
Table of Contents
1. Background
2. Modification of DNDC-Rice model
3. Model Varidation
4. Summary
1.
Background
2.
Modification of DNDC-Rice model
3.
Model Varidation
DNDC model for rice paddy fields
DNDC model for rice paddy fields
1992: A DNDC model was developed by Li et al. (1992) • Process-based model for agroecosystems
simulates carbon and nitrogen dynamics based on biogeochemical processes
Non-flooded agricultural conditions • Carbon sequestration
• GHGs (N2 O, CH4 , CO2 , NO and NH3 )
2004: Anaerobic biogeochemistry was incorporated for rice paddy fields (Li et al. 2004)
2008: DNDC 8.2 was modified for paddy ecosystems by Fumoto et al. (2008) →DNDC-Rice model
2009: A regional scale evaluation of CH4 emission using the
1992: A DNDC model was developed by Li et al. (1992)
• Process-based model for agroecosystems
simulates carbon and nitrogen dynamics based on biogeochemical processes
Non-flooded agricultural conditions
• Carbon sequestration
• GHGs (N2 O, CH4 , CO2 , NO and NH3 )
2004: Anaerobic biogeochemistry was incorporated for rice
paddy fields (Li et al. 2004)
2008: DNDC 8.2 was modified for paddy ecosystems by
Fumoto et al. (2008) →DNDC-Rice model
2009: A regional scale evaluation of CH4 emission using the
Outline
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Schematic description of the soil biogeochemistry sub-model of DNDC-Rice (Fumoto et al. 2008 and 2009)
Schematic description of the soil biogeochemistry sub-model of DNDC-Rice (Fumoto et al. 2008 and 2009)
O2 Diffusion Diffusion H2 CO2 CO2 CH4 Fe2+, Mn2+ Fe3+, Mn4+ DOC
Modification
Schematic description of the soil biogeochemistry sub-model of DNDC-Rice
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O
2diffusion to soil
O
2diffusion to soil
Modification
Cs Cs Max Crack Depth (m)O2 diffusion from four rateral faces Crack_factor = 4/Cs * h
O2 diffusion from surface
Cs: crack space (m)
h: thickness of a layer (m)
(Fumoto et al. 2008)
Gas diffusivity model – Osozawa 1987
Gas diffusivity model – Osozawa 1987
Osozawa (1987)Di = D0 εi 2.7
Di : O2 -air diffusion coefficient in soil (cm2 sec-1)
D0 : O2 -air diffusion coefficient in air at 20℃, 1 atm (=0.201 cm2 sec-1)
εi : gas phase (m3 m-3)
Osozawa (1987)
Di = D0 εi 2.7
Di : O2 -air diffusion coefficient in soil (cm2 sec-1)
D0 : O2 -air diffusion coefficient in air at 20℃, 1 atm (=0.201 cm2 sec-1)
εi : gas phase (m3 m-3)
(Fumoto et al. 2008 and 2009)
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Gas diffusivity model – BBC model
Gas diffusivity model – BBC model
Backingham-Burdine-Campbell (BBC) model (Moldrup et al. 1999, Rolston and Moldrup 2002)
Di = D0,T φi 2 (φ
i /εi ) 2+3/b
D0,T = D0,20 ((273+T)/(273+20))1.72 b = 13.6 clay + 3.5
Di : O2 -air diffusion coefficient in soil (cm2 sec-1)
D0, T : O2 -air diffusion coefficient in air at T ℃, 1 atm (cm2 sec-1)
D0, 20 : O2 -air diffusion coefficient in air at 20 ℃, 1 atm (=0.201 cm2 sec-1)
φi : porosity (m3 m-3)
εi : gas phase (m3 m-3)
b: campbell pore-size distribution parameter
Backingham-Burdine-Campbell (BBC) model
(Moldrup et al. 1999, Rolston and Moldrup 2002)
Di = D0,T φi2 (φ
i /εi ) 2+3/b
D0,T = D0,20 ((273+T)/(273+20))1.72 b = 13.6 clay + 3.5
Di : O2 -air diffusion coefficient in soil (cm2 sec-1)
D0, T : O2 -air diffusion coefficient in air at T ℃, 1 atm (cm2 sec-1)
D0, 20 : O2 -air diffusion coefficient in air at 20 ℃, 1 atm (=0.201 cm2 sec-1)
φi : porosity (m3 m-3) εi : gas phase (m3 m-3)
b: campbell pore-size distribution parameter
Other changes
Other changes
Decomposition factor (DRF) was changed from 0.82 to 0.2. Water table estimation
• Water table was estimated using simulated WFPS values of each 2cm depth soil.
Assumption1:
water content ≧ 0.94 Æ saturated water content < 0.94 Æ unsaturated Assumption2:
There is the water table at the top layer of the saturated layers.
Decomposition factor (DRF) was changed from 0.82 to 0.2.
Water table estimation
• Water table was estimated using simulated WFPS
values of each 2cm depth soil. Assumption1:
water content ≧ 0.94 Æ saturated water content < 0.94 Æ unsaturated
Assumption2:
There is the water table at the top layer of the saturated layers.
Modification
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Table of Contents
Table of Contents
1. Background
2. Modification of DNDC-Rice model
3. Model Validation
4. Summary
1.
Background
2.
Modification of DNDC-Rice model
3.
Model Validation
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A pot experiment conducted in a screenhouse, IRRI
A pot experiment conducted in a screenhouse, IRRI
Size of the pot
700 mm height and 530 mm i.d. Bulk density (0-15 cm)
0.82±0.53(Mg m-3)
Percolation rate 1 (mm day-1)
Clay content 59%
Soil organic C cont. 2.4%
Soil pH 6.2
Soil texture Clay
Field water capacity 0.8 (WFPS) Wilting point 0.4(WFPS) Size of the pot
700 mm height and 530 mm i.d.
Bulk density (0-15 cm)
0.82±0.53(Mg m-3)
Percolation rate 1 (mm day-1)
Clay content 59%
Soil organic C cont. 2.4%
Soil pH 6.2 Soil texture Clay
Field water capacity 0.8 (WFPS)
Wilting point 0.4(WFPS)
Scheme of the pot management
Scheme of the pot management
Criteria: -30 kPa at 15 cm depth or water table become below 40 cm Criteria: -30 kPa at 15 cm depth or water table become below 40 cm ↑ Soil surface Standing Water Surface Water retention Layer depth Flooding Transplanting PSB Rc80 Harvest Continuously flooding Continuously flooding N fert. 40 kgN ha-1 Straw 4 t ha-1 N fert. 40 kgN ha-1 Straw 4 t ha-1
Puddling DrainageDrainage
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Measurement of CH
4and N
2O fluxes
Measurement of CH
4and N
2O fluxes
Gas sampling
• Closed-chamber method
Collected gas samples at 0, 15, and 30
minutes after closing a rid.
Gas analysis
• CH
4Gaschromatography with FID
• N
2O Gaschromatography with ECD
Calculation of gas fluxes
• Linear regression method
Gas sampling
•
Closed-chamber method
Collected gas samples at 0, 15, and 30
minutes after closing a rid.
Gas analysis
•
CH
4Gaschromatography with FID
•
N
2O Gaschromatography with ECD
Calculation of gas fluxes
•
Linear regression method
Meteorological data
Meteorological data
Site: IRRI wetland
• Daily maximum temperature
• Daily minimum temperature
• Solar radiation
※Precipitation was assumed zero because the
measurement was conducted in a
screenhouse.
Site: IRRI wetland
•
Daily maximum temperature
•
Daily minimum temperature
•
Solar radiation
※Precipitation was assumed zero because the
measurement was conducted in a
screenhouse.
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Am: mean value of observed values
Fi: Simulated value
Ai: Observed value
N: Number of sample
Statictics
Statictics
Root Mean Square Error (RMSE) Root Mean Square Error (RMSE)
0 10 20 30 40 0 20 40 60 80 100 0 10 20 30 40
Observed daily maximum and minimum temperature and solar radiation during the cropping period
Observed daily maximum and minimum temperature and solar radiation during the cropping period
DAT Temperature( ℃ ) Solar radiation (MJ m -2 )
Daily mean air temp.
Solar Radiation
PuddlingTransplant Harvest
Fertilizer
Validation
May 19
2007 Aug. 242007
Results
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0 20 40 60 80 100 -0.6 -0.4 -0.2 0 0.2 0 20 40 60 80 100 -0.6 -0.4 -0.2 0 0.2
Observed and simulated water table for continuously flooding and AWD
Observed and simulated water table for continuously flooding and AWD
Water Table (m) DAT Simuated value Simuated value Observed value Observed value Continuously flooding AWD
PuddlingTransplant Harvest
Fertilizer
Simulated daily O2 content at 10 cm depth soil under continuously flooding and
Simulated daily O2 content at 10 cm depth soil under continuously flooding and
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0 20 40 60 80 100 0 2 4 6 8 10 12 0 20 40 60 80 100 -0.20 0.2 0.4 0.6 0.81
Observed and simulated daily CH4 and N2 O fluxes under continuously flooding (DRF=0.2)
Observed and simulated daily CH4 and N2 O fluxes under continuously flooding (DRF=0.2) CH 4 flux (kg C ha -1 d -1 )
TransplantFertilizer Harvest
Puddling N 2 O flux (kg N ha -1 d -1 ) DAT
Validation
ResultsSimulated (before modification)
Simulated (before modification)
0 20 40 60 80 100 0 2 4 6 8 10 12 0 20 40 60 80 100 -0.20 0.2 0.4 0.6 0.81
Observed and simulated daily CH and N O fluxes under AWD irrigation
Observed and simulated daily CH and N O fluxes under AWD irrigation
DAT
TransplantFertilizer Harvest
Puddling CH 4 flux (kg C ha -1 d -1 ) N 2 O flux (kg N ha -1 d -1 )
Validation
ResultsSimulated (before modification)
Simulated (before modification)
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Observed and simulated CH4 and N2 O emission rates of paddy fields under continuously flooding and AWD during the cropping period
Observed and simulated CH4 and N2 O emission rates of paddy fields under continuously flooding and AWD during the cropping period
Validation
ResultsObserved value Modification
(mean , SE) Before After
Modification of calculation method for O2 diffusion improved accuracy of simulation results of CH4 and N2 O fluxes, even though more improvement must be added.
Modification of calculation method for O2 diffusion
improved accuracy of simulation results of CH4 and N2 O
fluxes, even though more improvement must be added.
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We are going to make more modification to the model using monitoring data collected in field.
We are going to make more modification to the
model using monitoring data collected in field.