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
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)
What am I looking at? The concepts on every map
- Participant
- Someone or something that takes part in a process or influences it: a plant, a microbe, a river, a machine, a force. Participants are the rows of a map.
- Resource
- Something a step uses or uses up: water, oxygen, sunlight, a tool. Each step has an arrow down to the resources it uses.
- Step
- One thing that happens in a process. Every step has at least one participant and carries evidence.
- Decision fork
- A step where the process can go several ways. Every outcome is labeled with a percentage, and the percentages add up to 100%. It is not limited to yes or no.
- Loop
- A line that carries the process back to an earlier step. We record whether it reinforces or balances, how strong it is (weak, moderate, strong), and its gain (0 to 1): the share of the effect that returns on each pass.
- Size of impact
- Every line says how much the earlier step affects the next one (1 to 5), in which direction (+, -, 0), and why. Thicker lines mean bigger impact.
- Evidence
- The support for a claim: a source and what it shows. Every step, line, change and vote needs it. Click any step or line to read its evidence.
- Boundary
- Where a process starts and where it ends. Every process, and every subprocess, has a start and an end.
- Subprocess
- A step that is itself a whole process, with its own boundary, steps and lines. Click a step marked ↘ to open it. Subprocesses nest as deep as the evidence goes.
- Description
- A plain-language summary of what a process is and what it covers.
- Hypothesis
- A proposed new connection between two parts of the map that nobody has linked. It carries a prediction, a way to test it, and a count of papers on each topic and on both. It is an unverified idea until someone tests it.
Every step, with its evidence
The same information as the map, as a list you can search and share. Click a participant or resource to see everywhere it appears.
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)