Water erosion is the most active process controlling soil formation and evolution, which can affect the redistribution of carbon between terrestrial, aquatic, and atmospheric ecosystems. Erosion-induced organic carbon dynamic process should not be missing in terrestrial carbon cycle simulations.
Scientists combine a spatially distributed sediment delivery model and biogeochemical model to estimate fluxes by water retrieved 25 April 2024 from https://phys.org/news/2024-04-scientists-combine-spatially-sediment-delivery.html
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