Advertisement

More Related Content

Viewers also liked(20)

Similar to Process-based modelling of peat greenhouse gas emissions in Indonesian peatlands(20)

Advertisement

More from CIFOR-ICRAF(20)

Recently uploaded(20)

Advertisement

Process-based modelling of peat greenhouse gas emissions in Indonesian peatlands

  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
  19. cifor.org forestsnews.cifor.org ForestsTreesAgroforestry.org THANK YOU! QUESTIONS???
Advertisement