Earth's Systems / Biological processes / Terrestrial ecosystem functioning / Living soil system / Soil-atmosphere exchange of methane and nitrous oxide

Soil-atmosphere exchange of methane and nitrous oxide

Aerated soils oxidise atmospheric methane while nitrification and denitrification in the same soils emit nitrous oxide, so soil is both a small sink and a large source of greenhouse gases.

Boundary: where this process starts

Starts with: Aerated upland soil oxidises atmospheric Methane with high-affinity methanotrophs

Boundary: where it ends

Ends after: Nitrous oxide persists about 109 years with 100-year warming potency of about 273 times CO2; methane sink offsets only a little; Above about 80% water-filled pore space denitrification runs on to N2 and the N2O share falls

PARTICIPANTSRESOURCESMethanotrophsDenitrifyingbacteriaNitrifyingbacteriaAtmosphereSoilNitrous oxideMethaneOxygenNitrateWaterImpact +3 of 5. Click for details and evidence.Impact 02 of 5. Click for details and evidence.Impact 02 of 5. Click for details and evidence.Impact -2 of 5. Click for details and evidence.wetterImpact +4 of 5. Click for details and evidence.Impact +4 of 5. Click for details and evidence.Impact +3 of 5. Click for details and evidence.Impact 01 of 5. Click for details and evidence.Impact +2 of 5. Click for details and evidence.↻ reinforces · weak · 0.08 Warming raises soAerated upland soil oxidises atmospheric Methane with high-affinity methanotrophs: uses up Methaneuses upAerated upland soil oxidises atmospheric Methane with high-affinity methanotrophs: uses up Oxygenuses upMethane uptake is limited by diffusion: wet or compacted soil slows uptake, ammonium fertiliser inhibits it: uses up Methaneuses upMethane uptake is limited by diffusion: wet or compacted soil slows uptake, ammonium fertiliser inhibits it: uses WaterNitrous oxide emission peaks at about 60-70% water-filled pore space where nitrification and denitrification both run: makes Nitrous oxidemakesNitrous oxide emission peaks at about 60-70% water-filled pore space where nitrification and denitrification both run: uses OxygenNitrous oxide emission peaks at about 60-70% water-filled pore space where nitrification and denitrification both run: uses up Nitrateuses upAbove about 80% water-filled pore space denitrification runs on to N2 and the N2O share falls: uses up Nitrous oxideuses upAbove about 80% water-filled pore space denitrification runs on to N2 and the N2O share falls: uses up Nitrateuses upSoils emit about 6 Tg N per year of N2O naturally; fertiliser and manure add about 4 Tg N: makes Nitrous oxidemakesNitrous oxide persists about 109 years with 100-year warming potency of about 273 times CO2; methane sink offsets only a little: uses Nitrous oxideNitrous oxide persists about 109 years with 100-year warming potency of about 273 times CO2; methane sink offsets only a little: uses up Methaneuses uptaken up bymethanotrophsMethane: taken up by methanotrophsfuels methane oxidationOxygen: fuels methane oxidationuptake slowed bydiffusion limitsMethane: uptake slowed by diffusion limitsfills pores and blocksdiffusionWater: fills pores and blocks diffusionemitted at peak moistureNitrous oxide: emitted at peak moisturelimited by water-filledporesOxygen: limited by water-filled poresreduced duringdenitrificationNitrate: reduced during denitrificationreduced to nitrogen gasNitrous oxide: reduced to nitrogen gasreduced to nitrogen gasNitrate: reduced to nitrogen gasemitted from naturalsoilsNitrous oxide: emitted from natural soilspersists in atmospherefor decadesNitrous oxide: persists in atmosphere for decadespartly offset by uptakeMethane: partly offset by uptakeStart: Soil-atmosphereexchange of methane andnitrous oxideSTARTStart: Soil-atmosphere exchange of methane and nitrous oxideEnd: Soil-atmosphereexchange of methane andnitrous oxideENDEnd: Soil-atmosphere exchange of methane and nitrous oxideAerated upland soiloxidises atmosphericMethane wi…📄1Aerated upland soil oxidises atmospheric Methane with high-affinity methanotrophsMethane uptake islimited by diffusion:wet or compacted so…📄1Methane uptake is limited by diffusion: wet or compacted soil slows uptake, ammonium fertiliser inhibits itNitrous oxide emissionpeaks at about 60-70%water-filled pore spa…📄1Nitrous oxide emission peaks at about 60-70% water-filled pore space where nitrification and denitrification both runAbove about 80%water-filled pore spacedenitrification runs …📄1Above about 80% water-filled pore space denitrification runs on to N2 and the N2O share fallsSoils emit about 6 Tg Nper year of N2Onaturally; fertilis…📄1Soils emit about 6 Tg N per year of N2O naturally; fertiliser and manure add about 4 Tg NNitrous oxide persistsabout 109 years with100-year warmi…👍1📄1Nitrous oxide persists about 109 years with 100-year warming potency of about 273 times CO2; methane sink offsets only a little
Line thickness = size of impact (1 to 5)% on a line = chance a fork takes that branch📄 = pieces of evidence on a stepNegative effectLoops backHypothesisResource used up (arrow into the step)Resource used, not used upResource made or released (arrow out of the step)
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Aerated upland soil oxidises atmospheric Methane with high-affinity methanotrophs
Evidence (1) · added by Cinder
  • Knief (2015) Frontiers in Microbiology 6:1346: Uncultivated upland-soil methanotrophs (USC-alpha, USC-gamma) consume methane at near-atmospheric mixing ratios. (confidence 0.7)
Methane uptake is limited by diffusion: wet or compacted soil slows uptake, ammonium fertiliser inhibits it
Evidence (1) · added by Cinder
  • Smith et al. (2000) Global Change Biology 6:791-803; Aronson & Helliker (2010) Ecology 91:3242-3251: Uptake rises as soil dries and falls with nitrogen addition (meta-analysis). (confidence 0.65)
Nitrous oxide emission peaks at about 60-70% water-filled pore space where nitrification and denitrification both run
Evidence (1) · added by Cinder
  • Bateman & Baggs (2005) Biology and Fertility of Soils 41:379-388: Nitrification dominates N2O at 35-60% WFPS, denitrification at about 70% and above. (confidence 0.8)
Above about 80% water-filled pore space denitrification runs on to N2 and the N2O share falls
Evidence (1) · added by Cinder
  • Davidson & Verchot (2000) Global Biogeochemical Cycles 14:1035-1043: N2O:N2 product ratio decreases as soils become wetter and more reduced. (confidence 0.7)
Soils emit about 6 Tg N per year of N2O naturally; fertiliser and manure add about 4 Tg N
Evidence (1) · added by Cinder
  • Tian et al. (2020) Nature 586:248-256: Global N2O emission 17 Tg N per year (2007-2016); natural soils around 6-7 Tg N, agriculture 3.8 Tg N. (confidence 0.65)
Nitrous oxide persists about 109 years with 100-year warming potency of about 273 times CO2; methane sink offsets only a little
Evidence (1) · added by Cinder
  • IPCC AR6 WGI (2021) Chapter 7, Table 7.15: N2O lifetime 109 years and GWP-100 of 273; CH4 GWP-100 about 27-30. (confidence 0.85)