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Process-based modelling of greenhouse
gas emissions from oil palm plantations
in an Indonesian peatland
Erin Swails, Kristell Hergoualc’h, Jia Deng, Steve Frolking
Annual Meeting of the Society of Wetland Scientists, 1 – 10 June 2021
Tropical peatlands
• Extremely high soil C stocks –
total 350 Gt over 110 Mha
(Gumbricht et al 2017)
• Poor drainage → soil
waterlogging and SOC
accumulation
• Global extent - Southeast
Asia, Africa, South and
Central America
Planas Clarke et al. 2020
Land-use conversion in Southeast Asian peatlands
Miettinen et al. 2016
GHG emissions from Indonesian peatlands
Deforestation Burning Oil Palm Plantation
Drainage
Peat Forest
b
• Land-use conversion increases GHG emissions from peat
soils (Leifeld et al 2019, Hergoualc’h & Verchot 2014)
Peat GHG emissions
• OP peat emissions primarily released as CO2 (Swails et al 2021)
(Drösler et al 2014)
Data for estimation of peat GHG emissions
• 2013 IPCC supplement on wetlands: 1st
detailed GHG emission factors for tropical
peatlands
• EF based on data from Southeast Asia
(Hergoualc’h & Verchot 2014)
• Limited data for OP EF primarily based on
young plantations
• Process-based models can extrapolate point-
based measurements to larger regions over
extended time periods
Can DNDC simulate tropical peat GHG emissions?
• DeNitrification DeComposition (DNDC): 1-D process-based
model of C and N biogeochemistry
• Adapted for agricultural ecosystems, forests, and wetlands
Test site: Field measurements
• Permanent plots in smallholder oil palm plantations
(n=3) on peat
• Three years monthly measurements
o Peat GHG flux (total soil respiration, CH4, N2O)
o Controlling factors (water table, soil moisture + temp)
• Heterotrophic respiration estimated w/ site-specific
partitioning ratios
Modelling GHG fluxes and biogeophysical drivers
• Initialization – on-site measurements and literature-
based values
• Forcing
o Daily weather data from airport
o Management: planting, fertilization, harvest
• Calibration – vegetation growth, hydrology, SOC sub-
pools
• Testing – annual average peat GHG fluxes (total and
heterotrophic soil respiration, N2O, CH4)
• 30-year model runs – CP/FP simulations in each plot
• Up-scale outputs to plot level w/ spatial ratios
Calibration results: OP standing biomass,
litterfall, root mortality
• DNDC vegetation outputs fell within range of values
reported in the literature
Calibration results: Water table level
• DNDC adequately simulated WT fluctuations
OP1 OP2 OP3
Calibration results: Soil water-filled pore space
• DNDC adequately simulated fluctuations and micro-
spatial variation in soil WFPS
OP1 OP2 OP3
Calibration results: Soil temperature
• DNDC did not simulate the influence of vegetation
shading on soil temperature
OP1 OP2 OP3
closed canopy open canopy
intermediate
Calibration results: SOC sub-pools
• DNDC simulated the magnitude of total soil respiration
well overall
OP1 OP2 OP3
Model test results: Total and heterotrophic soil
respiration
RMSD = 3.0 Mg CO2-C ha-1 yr-1 RMSD = 4.0 Mg CO2-C ha-1 yr-1
Observed mean annual SR kg CO2-C ha-1 d-1
Predicted
mean
annual
SR
kg
CO
2
-C
ha
-1
d
-1
Observed mean annual SRh kg CO2-C ha-1 d-1
Predicted
mean
annual
SRh
kg
CO
2
-C
ha
-1
d
-1
What are long-term net CO2 emissions from peat
decomposition in OP plantations?
• Modelled net peat CO2 emissions declined
over time
IPCC
DNDC: yr 0 - 10
DNDC: yr 10 - 20
DNDC: yr 20 - 30
heterotrophic respiration
root mortality
litterfall
Takeaways and next steps
• Total soil respiration and biogeophysical
drivers were simulated reasonably well in
model runs, but..
o Heterotrophic respiration in our young OP
plantations was overestimated
• Model simulations indicate IPCC default
overestimates net CO2 emissions from peat
decomposition in older OP plantations
Takeaways and next steps
• Improve simulation of soil temperature
• Refine SOC sub-pool partitioning and spatial
representation of near/far conditions in OP
model simulations
• Use DNDC to investigate relationships between
GHG fluxes and potential proxies
• Model peat GHG emissions in forest
cifor.org
forestsnews.cifor.org
ForestsTreesAgroforestry.org
THANK YOU! QUESTIONS???

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Contributions of CH4 and N2O to peat GHG emissions from forest and oil palm plantations in an Indonesian peatland

  • 1. Process-based modelling of greenhouse gas emissions from oil palm plantations in an Indonesian peatland Erin Swails, Kristell Hergoualc’h, Jia Deng, Steve Frolking Annual Meeting of the Society of Wetland Scientists, 1 – 10 June 2021
  • 2. Tropical peatlands • Extremely high soil C stocks – total 350 Gt over 110 Mha (Gumbricht et al 2017) • Poor drainage → soil waterlogging and SOC accumulation • Global extent - Southeast Asia, Africa, South and Central America Planas Clarke et al. 2020
  • 3. Land-use conversion in Southeast Asian peatlands Miettinen et al. 2016
  • 4. GHG emissions from Indonesian peatlands Deforestation Burning Oil Palm Plantation Drainage Peat Forest b • Land-use conversion increases GHG emissions from peat soils (Leifeld et al 2019, Hergoualc’h & Verchot 2014)
  • 5. Peat GHG emissions • OP peat emissions primarily released as CO2 (Swails et al 2021) (Drösler et al 2014)
  • 6. Data for estimation of peat GHG emissions • 2013 IPCC supplement on wetlands: 1st detailed GHG emission factors for tropical peatlands • EF based on data from Southeast Asia (Hergoualc’h & Verchot 2014) • Limited data for OP EF primarily based on young plantations • Process-based models can extrapolate point- based measurements to larger regions over extended time periods
  • 7. Can DNDC simulate tropical peat GHG emissions? • DeNitrification DeComposition (DNDC): 1-D process-based model of C and N biogeochemistry • Adapted for agricultural ecosystems, forests, and wetlands
  • 8. Test site: Field measurements • Permanent plots in smallholder oil palm plantations (n=3) on peat • Three years monthly measurements o Peat GHG flux (total soil respiration, CH4, N2O) o Controlling factors (water table, soil moisture + temp) • Heterotrophic respiration estimated w/ site-specific partitioning ratios
  • 9. Modelling GHG fluxes and biogeophysical drivers • Initialization – on-site measurements and literature- based values • Forcing o Daily weather data from airport o Management: planting, fertilization, harvest • Calibration – vegetation growth, hydrology, SOC sub- pools • Testing – annual average peat GHG fluxes (total and heterotrophic soil respiration, N2O, CH4) • 30-year model runs – CP/FP simulations in each plot • Up-scale outputs to plot level w/ spatial ratios
  • 10. Calibration results: OP standing biomass, litterfall, root mortality • DNDC vegetation outputs fell within range of values reported in the literature
  • 11. Calibration results: Water table level • DNDC adequately simulated WT fluctuations OP1 OP2 OP3
  • 12. Calibration results: Soil water-filled pore space • DNDC adequately simulated fluctuations and micro- spatial variation in soil WFPS OP1 OP2 OP3
  • 13. Calibration results: Soil temperature • DNDC did not simulate the influence of vegetation shading on soil temperature OP1 OP2 OP3 closed canopy open canopy intermediate
  • 14. Calibration results: SOC sub-pools • DNDC simulated the magnitude of total soil respiration well overall OP1 OP2 OP3
  • 15. Model test results: Total and heterotrophic soil respiration RMSD = 3.0 Mg CO2-C ha-1 yr-1 RMSD = 4.0 Mg CO2-C ha-1 yr-1 Observed mean annual SR kg CO2-C ha-1 d-1 Predicted mean annual SR kg CO 2 -C ha -1 d -1 Observed mean annual SRh kg CO2-C ha-1 d-1 Predicted mean annual SRh kg CO 2 -C ha -1 d -1
  • 16. What are long-term net CO2 emissions from peat decomposition in OP plantations? • Modelled net peat CO2 emissions declined over time IPCC DNDC: yr 0 - 10 DNDC: yr 10 - 20 DNDC: yr 20 - 30 heterotrophic respiration root mortality litterfall
  • 17. Takeaways and next steps • Total soil respiration and biogeophysical drivers were simulated reasonably well in model runs, but.. o Heterotrophic respiration in our young OP plantations was overestimated • Model simulations indicate IPCC default overestimates net CO2 emissions from peat decomposition in older OP plantations
  • 18. Takeaways and next steps • Improve simulation of soil temperature • Refine SOC sub-pool partitioning and spatial representation of near/far conditions in OP model simulations • Use DNDC to investigate relationships between GHG fluxes and potential proxies • Model peat GHG emissions in forest