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

PARTICIPANTSRESOURCESIron oxidesIron-reducingbacteriaPhenol oxidaseSoil waterSoil poresOxygenIron oxidesIronSoil organicmatterPhosphateImpact +3 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 +4 of 5. Click for details and evidence.Impact +3 of 5. Click for details and evidence.drainage or root oxygen retuImpact +3 of 5. Click for details and evidence.Impact +3 of 5. Click for details and evidence.Impact -3 of 5. Click for details and evidence.↻ reinforces · weak · 0.15 Released carbon fWater fills pores, gas diffuses about 10,000 times more slowly than in air, interior microsites go anoxic: uses up Oxygenuses upIron-reducing bacteria use Fe(III) oxides as electron acceptor, dissolving them: uses up Iron oxidesuses upIron-reducing bacteria use Fe(III) oxides as electron acceptor, dissolving them: makes IronmakesIron-reducing bacteria use Fe(III) oxides as electron acceptor, dissolving them: uses up Soil organic matteruses upDissolving oxides releases sorbed phosphate and organic carbon: makes PhosphatemakesAnoxia suppresses phenol oxidase; phenolics build up and inhibit hydrolases (enzyme latch): uses Soil organic matterFe(II) diffuses to oxic zones and reoxidises, forming new oxides that re-sorb phosphate and carbon: uses up Oxygenuses upFe(II) diffuses to oxic zones and reoxidises, forming new oxides that re-sorb phosphate and carbon: makes Iron oxidesmakesFe(II) diffuses to oxic zones and reoxidises, forming new oxides that re-sorb phosphate and carbon: uses up Ironuses upFe(II) diffuses to oxic zones and reoxidises, forming new oxides that re-sorb phosphate and carbon: uses up Phosphateuses upconsumed faster thansuppliedOxygen: consumed faster than supplieddissolved as electronacceptorsIron oxides: dissolved as electron acceptorsreleased as Fe2+Iron: released as Fe2+consumed as electrondonorSoil organic matter: consumed as electron donorreleased from dissolvingoxidesPhosphate: released from dissolving oxidesprotected fromdecompositionSoil organic matter: protected from decompositionused in reoxidationOxygen: used in reoxidationreform as new solidsIron oxides: reform as new solidsreoxidized in oxic zonesIron: reoxidized in oxic zonesresorbed onto new oxidesPhosphate: resorbed onto new oxidesStart: Iron redoxcycling and the enzymelatch in wet soilSTARTStart: Iron redox cycling and the enzyme latch in wet soilEnd: Iron redox cyclingand the enzyme latch inwet soilENDEnd: Iron redox cycling and the enzyme latch in wet soilWater fills pores, gasdiffuses about 10,000times more slowly th…📄1Water fills pores, gas diffuses about 10,000 times more slowly than in air, interior microsites go anoxicIron-reducing bacteriause Fe(III) oxides aselectron accepto…📄1Iron-reducing bacteria use Fe(III) oxides as electron acceptor, dissolving themDissolving oxidesreleases sorbedphosphate and organ…📄1Dissolving oxides releases sorbed phosphate and organic carbonAnoxia suppressesphenol oxidase;phenolics build up a…👍1📄1Anoxia suppresses phenol oxidase; phenolics build up and inhibit hydrolases (enzyme latch)Fe(II) diffuses to oxiczones and reoxidises,forming new oxides th…📄1Fe(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)