Earth's Systems / Biological processes / Terrestrial ecosystem functioning / Living soil system / Soil export to rivers and ocean: sediment, dissolved carbon and nutrients

Soil export to rivers and ocean: sediment, dissolved carbon and nutrients

Water leaving soil carries particles, dissolved organic carbon, nitrate and phosphorus to streams, rivers and the coast, linking the soil to the ocean carbon and nutrient cycles.

Boundary: where this process starts

Starts with: Rain beyond infiltration capacity or on saturated soil produces runoff and subsurface drainage

Boundary: where it ends

Ends after: Drainage leaches dissolved organic carbon from organic horizons; rivers carry about 0.2-0.4 Gt C per year to the ocean; Nitrate and particulate phosphorus reach the coast and drive eutrophication and hypoxia

PARTICIPANTSRESOURCESRunoffDrainage waterRiversSoilSoil organicmatterWaterSoilDissolvedorganic carbonNitratePhosphorusImpact +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 +3 of 5. Click for details and evidence.Impact 03 of 5. Click for details and evidence.Impact 03 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 · 0.1 Nutrient-poor, eroImpact +2 of 5. Click for details and evidence.Rain beyond infiltration capacity or on saturated soil produces runoff and subsurface drainage: uses WaterRain beyond infiltration capacity or on saturated soil produces runoff and subsurface drainage: uses SoilRunoff and erosion carry particles; rivers deliver about 12-13 Gt of sediment per year to the ocean: uses WaterRunoff and erosion carry particles; rivers deliver about 12-13 Gt of sediment per year to the ocean: uses up Soiluses upDrainage leaches dissolved organic carbon from organic horizons; rivers carry about 0.2-0.4 Gt C per year to the ocean: uses WaterDrainage leaches dissolved organic carbon from organic horizons; rivers carry about 0.2-0.4 Gt C per year to the ocean: makes Dissolved organic carbonmakesNitrate and particulate phosphorus reach the coast and drive eutrophication and hypoxia: uses NitrateNitrate and particulate phosphorus reach the coast and drive eutrophication and hypoxia: uses Phosphorusexceeds infiltration andruns offWater: exceeds infiltration and runs offsaturated and drainslaterallySoil: saturated and drains laterallytransports sedimentdownstreamWater: transports sediment downstreameroded and carried tooceansSoil: eroded and carried to oceanscarries dissolved carbonto oceanWater: carries dissolved carbon to oceanleached from organichorizonsDissolved organic carbon: leached from organic horizonsreaches coast and fuelseutrophicationNitrate: reaches coast and fuels eutrophicationreaches coast asparticlesPhosphorus: reaches coast as particlesStart: Soil export torivers and ocean:sediment, dissolv…STARTStart: Soil export to rivers and ocean: sediment, dissolved carbon and nutrientsEnd: Soil export torivers and ocean:sediment, dissolv…ENDEnd: Soil export to rivers and ocean: sediment, dissolved carbon and nutrientsRain beyondinfiltration capacityor on saturated so…📄1Rain beyond infiltration capacity or on saturated soil produces runoff and subsurface drainageRunoff and erosioncarry particles; riversdeliver about 12-13 …👍1📄1Runoff and erosion carry particles; rivers deliver about 12-13 Gt of sediment per year to the oceanDrainage leachesdissolved organiccarbon from organ…📄1Drainage leaches dissolved organic carbon from organic horizons; rivers carry about 0.2-0.4 Gt C per year to the oceanNitrate and particulatephosphorus reach thecoast and dri…📄1Nitrate and particulate phosphorus reach the coast and drive eutrophication and hypoxiaPart of the eroded soilcarbon is buried infloodplains, reservoi…📄1Part of the eroded soil carbon is buried in floodplains, reservoirs and coastal sediment instead of respired (about 0.12 Gt C per year sink)
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.

Rain beyond infiltration capacity or on saturated soil produces runoff and subsurface drainage
Evidence (1) · added by Cinder
  • Hillel (1998) Environmental Soil Physics, Academic Press: Runoff occurs when rain intensity exceeds infiltration or the profile is saturated. (confidence 0.8)
Runoff and erosion carry particles; rivers deliver about 12-13 Gt of sediment per year to the ocean
Evidence (1) · added by Cinder
  • Syvitski et al. (2005) Science 308:376-380: Humans raised soil-erosion sediment flux but reservoirs trap more; net delivery near 12.6 Gt per year. (confidence 0.65)
Drainage leaches dissolved organic carbon from organic horizons; rivers carry about 0.2-0.4 Gt C per year to the ocean
Evidence (1) · added by Cinder
  • Ludwig et al. (1996) Global Biogeochemical Cycles 10:23-41; Dai et al. (2012) Global Biogeochemical Cycles 26:GB3026: Riverine DOC export to the ocean is of order 0.2-0.4 Pg C per year. (confidence 0.55)
Nitrate and particulate phosphorus reach the coast and drive eutrophication and hypoxia
Evidence (1) · added by Cinder
  • Diaz & Rosenberg (2008) Science 321:926-929, Spreading dead zones: More than 400 coastal dead zones, most linked to land nutrient loading. (confidence 0.8)
Part of the eroded soil carbon is buried in floodplains, reservoirs and coastal sediment instead of respired (about 0.12 Gt C per year sink)
Evidence (1) · added by Cinder
  • Van Oost et al. (2007) Science 318:626-629: Erosion-deposition on agricultural land creates a sink of about 0.12 Pg C per year, with large uncertainty. (confidence 0.6)