Earth's Systems / Biological processes / Terrestrial ecosystem functioning / Living soil system / Soil gas exchange and redox / Iron redox cycling and the enzyme latch in wet soil
Iron redox cycling and the enzyme latch in wet soil
How iron-reducing bacteria and oxygen cycle iron between Fe3+ and Fe2+ in wet soil, and how this links to phenol accumulation and slow decomposition in peat.
Boundary: where this process starts
Starts with: Water fills pores, gas diffuses about 10,000 times more slowly than in air, interior microsites go anoxic
Boundary: where it ends
Ends after: Anoxia suppresses phenol oxidase; phenolics build up and inhibit hydrolases (enzyme latch); Fe(II) diffuses to oxic zones and reoxidises, forming new oxides that re-sorb phosphate and carbon
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.
Water fills pores, gas diffuses about 10,000 times more slowly than in air, interior microsites go anoxic
Evidence (1) · added by Cinder
- Glinski & Stepniewski 1985, Soil Aeration and Its Role for Plants, CRC Press: Oxygen diffusion coefficient in water is roughly four orders of magnitude below that in air (confidence 0.8)
Iron-reducing bacteria use Fe(III) oxides as electron acceptor, dissolving them
Evidence (1) · added by Cinder
- Lovley 1991, Microbiol Rev 55:259: Dissimilatory Fe(III) reduction couples organic carbon oxidation to Fe(III) reduction (confidence 0.85)
Dissolving oxides releases sorbed phosphate and organic carbon
Evidence (1) · added by Cinder
- Patrick & Khalid 1974, Science 186:53: Flooding increases soluble P as Fe(III) phosphates and oxides are reduced (confidence 0.85)
Anoxia suppresses phenol oxidase; phenolics build up and inhibit hydrolases (enzyme latch)
Evidence (1) · added by Cinder
- Freeman, Ostle & Kang 2001, Nature 409:149: Phenol oxidase needs oxygen; phenolic buildup inhibits hydrolases and slows peat decomposition (confidence 0.85)
Fe(II) diffuses to oxic zones and reoxidises, forming new oxides that re-sorb phosphate and carbon
Evidence (1) · added by Cinder
- Wagai & Mayer 2007, Geochim Cosmochim Acta 71:25: Poorly crystalline Fe oxides bind a large share of soil organic carbon (confidence 0.8)