Plant-mediated water flux

Transpiration is the dominant part of evapotranspiration; roots also move water between wet and dry soil layers, extending the time plants can stay active.

Boundary: where this process starts

Starts with: Transpiration is 80-90% of evapotranspiration

Boundary: where it ends

Ends after: Wetter deep soil supports deeper roots and more uptake

PARTICIPANTSRESOURCESPlantsPlant rootsWaterWater vapourImpact +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.Impact +3 of 5. Click for details and evidence.↻ reinforces · weak · 0.15 deep water accessTranspiration is 80-90% of evapotranspiration: uses WaterTranspiration is 80-90% of evapotranspiration: makes Water vapourmakesHydraulic redistribution moves water through roots: uses WaterWetter deep soil supports deeper roots and more uptake: uses Waterlost through leafstomataWater: lost through leaf stomatareleased astranspirationWater vapour: released as transpirationmoved through roots atnightWater: moved through roots at nightstored in deeper soillayersWater: stored in deeper soil layersStart: Plant-mediatedwater fluxSTARTStart: Plant-mediated water fluxEnd: Plant-mediatedwater fluxENDEnd: Plant-mediated water fluxTranspiration is 80-90%of evapotranspiration📄1Transpiration is 80-90% of evapotranspirationHydraulicredistribution moveswater through roots📄1Hydraulic redistribution moves water through rootsWetter deep soilsupports deeper rootsand more uptake📄1Wetter deep soil supports deeper roots and more uptake
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.

Transpiration is 80-90% of evapotranspiration
Evidence (1) · added by Broad
  • Jasechko 2013, Terrestrial water fluxes dominated by transpiration, Nature, doi:10.1038/nature11983: Isotope-based global estimate: transpiration is about 80-90% of terrestrial ET. (confidence 0.75)
Hydraulic redistribution moves water through roots
Evidence (1) · added by Broad
  • Neumann & Cardon 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 redistribution moves substantial volumes of water between soil layers at night. (confidence 0.75)
Wetter deep soil supports deeper roots and more uptake
Evidence (1) · added by Broad
  • Schenk & Jackson 2002, The global biogeography of roots, Ecological Monographs, doi:10.1890/0012-9615(2002)072[0311:tgbor]2.0.co;2: Root depth tracks water availability. (confidence 0.6)