Earth's Systems / Biological processes / Terrestrial ecosystem functioning / Water movement / Hydraulic redistribution by roots (0.04-1.3 mm per day)

Hydraulic redistribution by roots (0.04-1.3 mm per day)

Roots act as passive conduits that move water along water-potential gradients, usually from wet deep soil to dry shallow soil at night (hydraulic lift) and sometimes downward after rain, buffering drought for plants and soil microbes.

Boundary: where this process starts

Starts with: Night: stomata close and roots lift water from wet subsoil to dry topsoil

Boundary: where it ends

Ends after: Topsoil nutrient uptake increases and plant water status improves; Daytime transpiration pulls water back out of shallow layers

PARTICIPANTSRESOURCESRootsPlantsMycorrhizalfungiSoilBacteriaWaterNitrogenPhosphorusImpact +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.Impact +3 of 5. Click for details and evidence.↻ reinforces · weak · 0.2 deeper stores drawImpact +3 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.Night: stomata close and roots lift water from wet subsoil to dry topsoil: uses WaterRedistributed water keeps topsoil roots, hyphae and microbes active in dry spells: uses WaterRedistributed water keeps topsoil roots, hyphae and microbes active in dry spells: uses NitrogenTopsoil nutrient uptake increases and plant water status improves: uses WaterTopsoil nutrient uptake increases and plant water status improves: uses up Nitrogenuses upTopsoil nutrient uptake increases and plant water status improves: uses up Phosphorususes upDaytime transpiration pulls water back out of shallow layers: uses up Wateruses upmoved upward into drytopsoilWater: moved upward into dry topsoilkeeps topsoil biotahydratedWater: keeps topsoil biota hydratedaccessed by shallowrootsNitrogen: accessed by shallow rootsimproves plant waterstatusWater: improves plant water statustaken up from topsoilNitrogen: taken up from topsoiltaken up from topsoilPhosphorus: taken up from topsoilpulled out of shallowlayersWater: pulled out of shallow layersStart: Hydraulicredistribution by roots(0.04-1.3 mm per day)STARTStart: Hydraulic redistribution by roots (0.04-1.3 mm per day)End: Hydraulicredistribution by roots(0.04-1.3 mm per day)ENDEnd: Hydraulic redistribution by roots (0.04-1.3 mm per day)Night: stomata closeand roots lift waterfrom wet subsoil to d…👍1📄1Night: stomata close and roots lift water from wet subsoil to dry topsoilRedistributed waterkeeps topsoil roots,hyphae and microb…📄1 ↗1Redistributed water keeps topsoil roots, hyphae and microbes active in dry spellsTopsoil nutrient uptakeincreases and plantwater status improves📄1Topsoil nutrient uptake increases and plant water status improvesDaytime transpirationpulls water back out ofshallow layers📄1Daytime transpiration pulls water back out of shallow layers
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

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Night: stomata close and roots lift water from wet subsoil to dry topsoil
Evidence (1) · added by Quanta
  • Neumann 2012, The magnitude of hydraulic redistribution by plant roots: a review and synthesis, New Phytologist, doi:10.1111/j.1469-8137.2012.04088.x: Hydraulic lift occurs when transpiration stops and upper soil is drier than deep roots; magnitude 0.04-1.3 mm/day. (confidence 0.6)
Redistributed water keeps topsoil roots, hyphae and microbes active in dry spells
Evidence (1) · added by Quanta
  • Neumann 2012, The magnitude of hydraulic redistribution by plant roots: a review and synthesis, New Phytologist, doi:10.1111/j.1469-8137.2012.04088.x: Redistributed water supports nutrient uptake and microbial activity in dry topsoil; review notes ecological significance. (confidence 0.5)
Topsoil nutrient uptake increases and plant water status improves
Evidence (1) · added by Quanta
  • Neumann 2012, The magnitude of hydraulic redistribution by plant roots: a review and synthesis, New Phytologist, doi:10.1111/j.1469-8137.2012.04088.x: Improved root function in dry topsoil increases nutrient capture. (confidence 0.45)
Daytime transpiration pulls water back out of shallow layers
Evidence (1) · added by Quanta
  • Neumann 2012, The magnitude of hydraulic redistribution by plant roots: a review and synthesis, New Phytologist, doi:10.1111/j.1469-8137.2012.04088.x: Daytime reversal of flow; net gain is a fraction of transpiration (order 10-20 percent). (confidence 0.4)