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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

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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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4

Alternate Wetting and Drying

A

lternate

W

etting and

D

rying

ƒ A Water-saving irrigation technique for rice cropping ƒ AWD has been investigated by International Rice

Research Institute (IRRI) in Philippines since the early 1970’s.

ƒ With the technique:

• 15-30% unproductive water outflow can be cut down • Water productivity can be increased without

sacrificing yield.

ƒ 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

ƒ A Water-saving irrigation technique for rice cropping

ƒ AWD has been investigated by International Rice

Research Institute (IRRI) in Philippines since the early 1970’s.

ƒ With the technique:

• 15-30% unproductive water outflow can be cut down

• Water productivity can be increased without

sacrificing yield.

ƒ 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

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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 water

Irrigation 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

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AWD

AWD

Irrigation Water Plenty

Global warming potential

High 0

CH

4

CH

4

N

2

O

N

2

O

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

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DNDC model for rice paddy fields

DNDC model for rice paddy fields

ƒ 1992: A DNDC model was developed by Li et al. (1992) • Process-based model for agroecosystems

ƒ simulates carbon and nitrogen dynamics based on biogeochemical processes

ƒ Non-flooded agricultural conditions • Carbon sequestration

• GHGs (N2 O, CH4 , CO2 , NO and NH3 )

ƒ 2004: Anaerobic biogeochemistry was incorporated for rice paddy fields (Li et al. 2004)

ƒ 2008: DNDC 8.2 was modified for paddy ecosystems by Fumoto et al. (2008) →DNDC-Rice model

ƒ 2009: A regional scale evaluation of CH4 emission using the

ƒ 1992: A DNDC model was developed by Li et al. (1992)

• Process-based model for agroecosystems

ƒ simulates carbon and nitrogen dynamics based on biogeochemical processes

ƒ Non-flooded agricultural conditions

• Carbon sequestration

• GHGs (N2 O, CH4 , CO2 , NO and NH3 )

ƒ 2004: Anaerobic biogeochemistry was incorporated for rice

paddy fields (Li et al. 2004)

ƒ 2008: DNDC 8.2 was modified for paddy ecosystems by

Fumoto et al. (2008) →DNDC-Rice model

ƒ 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)

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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

2

diffusion to soil

O

2

diffusion 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)

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Gas diffusivity model – Osozawa 1987

Gas diffusivity model – Osozawa 1987

ƒ 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)

ƒ 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

ƒ Backingham-Burdine-Campbell (BBC) model (Moldrup et al. 1999, Rolston and Moldrup 2002)

Di = D0,T φi 2

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

ƒ Backingham-Burdine-Campbell (BBC) model

(Moldrup et al. 1999, Rolston and Moldrup 2002)

Di = D0,T φi2

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

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Other changes

Other changes

ƒ Decomposition factor (DRF) was changed from 0.82 to 0.2. ƒ Water table estimation

• Water table was estimated using simulated WFPS values of each 2cm depth soil.

ƒ Assumption1:

water content ≧ 0.94 Æ saturated water content < 0.94 Æ unsaturated ƒ Assumption2:

There is the water table at the top layer of the saturated layers.

ƒ Decomposition factor (DRF) was changed from 0.82 to 0.2.

ƒ Water table estimation

• Water table was estimated using simulated WFPS

values of each 2cm depth soil. ƒ Assumption1:

water content ≧ 0.94 Æ saturated water content < 0.94 Æ unsaturated

ƒ 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

ƒ Size of the pot

700 mm height and 530 mm i.d. ƒ Bulk density (0-15 cm)

0.82±0.53(Mg m-3)

ƒ Percolation rate 1 (mm day-1)

ƒ Clay content 59%

ƒ Soil organic C cont. 2.4%

ƒ Soil pH 6.2

ƒ Soil texture Clay

ƒ Field water capacity 0.8 (WFPS) ƒ Wilting point 0.4(WFPS) ƒ Size of the pot

700 mm height and 530 mm i.d.

ƒ Bulk density (0-15 cm)

0.82±0.53(Mg m-3)

ƒ Percolation rate 1 (mm day-1)

ƒ Clay content 59%

ƒ Soil organic C cont. 2.4%

ƒ Soil pH 6.2 ƒ Soil texture Clay

ƒ Field water capacity 0.8 (WFPS)

ƒ Wilting point 0.4(WFPS)

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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

4

and N

2

O fluxes

Measurement of CH

4

and N

2

O fluxes

ƒ Gas sampling

• Closed-chamber method

ƒ Collected gas samples at 0, 15, and 30

minutes after closing a rid.

ƒ Gas analysis

• CH

4

Gaschromatography with FID

• N

2

O Gaschromatography with ECD

ƒ Calculation of gas fluxes

• Linear regression method

ƒ

Gas sampling

Closed-chamber method

ƒ

Collected gas samples at 0, 15, and 30

minutes after closing a rid.

ƒ

Gas analysis

CH

4

Gaschromatography with FID

N

2

O Gaschromatography with ECD

ƒ

Calculation of gas fluxes

Linear regression method

(23)

Meteorological data

Meteorological data

ƒ Site: IRRI wetland

• Daily maximum temperature

• Daily minimum temperature

• Solar radiation

※Precipitation was assumed zero because the

measurement was conducted in a

screenhouse.

ƒ

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

ƒ Root Mean Square Error (RMSE)

ƒ Root Mean Square Error (RMSE)

(25)

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

(27)

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

Results

Simulated (before modification)

Simulated (before modification)

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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 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

Results

Simulated (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

Results

Observed value Modification

(mean , SE) Before After

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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.

32

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References

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