Sequential soil pH buffer systems

How soil pH is held in turn by carbonate, silicate and exchange, aluminium and iron oxide buffer systems, each active over its own pH range.

Boundary: where this process starts

Starts with: Carbonate buffer range (about pH 8.6 to 6.2): calcite dissolves and consumes acid

Boundary: where it ends

Ends after: Al3+ damages root tips and microbes, lowering uptake and biological activity

PARTICIPANTSRESOURCESCalciteClay mineralsAluminumIron oxidesSoil solutionOtherparticipantsHydrogen ionsAluminumCarbonateCalciumBase cationsImpact +3 of 5. Click for details and evidence.Impact -3 of 5. Click for details and evidence.calcite exhaustedImpact -3 of 5. Click for details and evidence.base cations depletedImpact -4 of 5. Click for details and evidence.Impact -3 of 5. Click for details and evidence.Impact -2 of 5. Click for details and evidence.↻ reinforces · weak · 0.15 Poor root and micCarbonate buffer range (about pH 8.6 to 6.2): calcite dissolves and consumes acid: uses up Hydrogen ionsuses upCarbonate buffer range (about pH 8.6 to 6.2): calcite dissolves and consumes acid: uses up Carbonateuses upCarbonate buffer range (about pH 8.6 to 6.2): calcite dissolves and consumes acid: makes CalciummakesSilicate and exchange buffer ranges (about pH 6.2 to 4.2): protons displace base cations: uses up Hydrogen ionsuses upSilicate and exchange buffer ranges (about pH 6.2 to 4.2): protons displace base cations: makes Base cationsmakesAluminum buffer range (about pH 4.2 to 3.0): Al hydroxides dissolve, releasing toxic Al3+: uses up Hydrogen ionsuses upAluminum buffer range (about pH 4.2 to 3.0): Al hydroxides dissolve, releasing toxic Al3+: makes AluminummakesAl3+ damages root tips and microbes, lowering uptake and biological activity: uses Aluminumneutralized by calcitedissolutionHydrogen ions: neutralized by calcite dissolutiondissolves to neutralizeacidCarbonate: dissolves to neutralize acidreleased into solutionCalcium: released into solutiondisplace base cationsfrom exchangeHydrogen ions: displace base cations from exchangedisplaced into solutionBase cations: displaced into solutionconsumed in dissolutionHydrogen ions: consumed in dissolutionreleased from hydroxidedissolutionAluminum: released from hydroxide dissolutiontoxic to roots andmicrobesAluminum: toxic to roots and microbesStart: Sequential soilpH buffer systemsSTARTStart: Sequential soil pH buffer systemsEnd: Sequential soil pHbuffer systemsENDEnd: Sequential soil pH buffer systemsCarbonate buffer range(about pH 8.6 to 6.2):calcite dissolves a…📄1Carbonate buffer range (about pH 8.6 to 6.2): calcite dissolves and consumes acidSilicate and exchangebuffer ranges (about pH6.2 to 4.2): proto…📄1Silicate and exchange buffer ranges (about pH 6.2 to 4.2): protons displace base cationsAluminum buffer range(about pH 4.2 to 3.0):Al hydroxides dissolv…📄1Aluminum buffer range (about pH 4.2 to 3.0): Al hydroxides dissolve, releasing toxic Al3+Al3+ damages root tipsand microbes, loweringuptake and biologic…📄1Al3+ damages root tips and microbes, lowering uptake and biological activity
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.

Carbonate buffer range (about pH 8.6 to 6.2): calcite dissolves and consumes acid
Evidence (1) · added by Cinder
  • Ulrich 1983 (Ulrich & Pankrath eds.): Carbonate buffering holds pH above about 6.2 until calcite is exhausted (confidence 0.75)
Silicate and exchange buffer ranges (about pH 6.2 to 4.2): protons displace base cations
Evidence (1) · added by Cinder
  • Ulrich 1983 (Ulrich & Pankrath eds.): Silicate weathering then cation exchange buffer between roughly pH 6.2 and 4.2 (confidence 0.7)
Aluminum buffer range (about pH 4.2 to 3.0): Al hydroxides dissolve, releasing toxic Al3+
Evidence (1) · added by Cinder
  • Ulrich 1983 (Ulrich & Pankrath eds.): Below pH about 4.2 Al hydroxides take up protons and release Al3+ (confidence 0.75)
Al3+ damages root tips and microbes, lowering uptake and biological activity
Evidence (1) · added by Cinder
  • Kochian, Hoekenga & Pineros 2004, Annu Rev Plant Biol 55:459: Al3+ inhibits root elongation and nutrient uptake in acid soils (confidence 0.85)