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Publication Date
1 January 2022

A Global Soil Erosion and Sediment Flux Model

Subtitle
Developing a global soil erosion and sediment flux model to advance understanding of land, river, and ocean geomorphology and biogeochemistry.
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Soil erosion plays a crucial role in global biogeochemical cycles and food security
Science

Soil erosion plays a crucial role in landscape evolution, global biogeochemical cycles, and food security, but it is rarely represented in Earth system models. As a result, these models do not fully capture the impact of climate and land use changes on land, river, and ocean geomorphology and biogeochemistry. A new study developed a global soil erosion and sediment flux model for Earth system modeling. The new model provides skillful simulations of soil erosion and sediment flux to produce credible predictions of land and river sediment dynamics in response to climate change and human disturbances.

Impact

Researchers implemented a new model of soil erosion and sediment flux in the Energy Exascale Earth System Model (E3SM). This study showed that conservation agriculture is an effective practice for reducing soil erosion in cropland, so its broader adoption in developing countries may improve sustainable food production. The study also showed that deforestation will rapidly increase river sediment in tropical river basins that currently have large rainforest coverage. The new capability allows E3SM to be used to evaluate the impact of climate and land use changes on land, river, and ocean geomorphology and biogeochemistry to improve modeling of the food-energy-water nexus.

Summary

Soil erosion produces enormous amounts of sediment, carbon, and nutrient fluxes from land to rivers. Historical records show that it is susceptible to climate change and cropland expansion. To predict soil erosion in the context of climate and land use changes, this study explicitly represents cropland management actions, like conservation agriculture, irrigation, and crop residue management, in the E3SM soil erosion model. The model also explicitly represents the impact of geological factors, such as lithology and glaciers, on soil erosion. The new model demonstrates good performance in simulating the spatial variability of global soil erosion and sediment flux. Compared with the two widely-used benchmark models, this model achieves better performance in predicting soil erosion in mountainous regions and representing the variability of sediment flux within river basins. The model simulations show that conservation agriculture reduced cropland soil erosion in countries where it is well-adopted, such as the United States and Argentina. In contrast, irrigation has increased soil erosion in many Asian countries. In tropical rainforest watersheds, sediment flux is limited by soil erosion instead of sediment transport. As a result, deforestation will increase river sediment rapidly in these watersheds.  

Point of Contact
L. Ruby Leung
Institution(s)
Pacific Northwest National Laboratory (PNNL)
Funding Program Area(s)
Publication