Abstract
Wind erosion, also known as eolian erosion, is a dynamic process by which soil particles are detached and displaced by the erosive forces of the wind. Wind erosion occurs when the force of wind exceeds the threshold level of soil’s resistance to erosion. Geological, anthropogenic, and climatic processes control the rate and magnitude of wind erosion (Fig. 3.1). Abrupt fluctuations in weather patterns trigger severe wind storms. Wind erosion is the result of complex interactions among wind intensity, precipitation, surface roughness, soil texture and aggregation, agricultural activities, vegetation cover, and field size. Plowed soils with low organic matter content and those intensively grazed and trampled upon are the most susceptible to erosion. About 50% of the dust clouds result from deforestation and agricultural activities (Gomes et al., 2003).
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Blanco-Canqui, H., Lal, R. (2010). Wind Erosion. In: Principles of Soil Conservation and Management. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-8709-7_3
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DOI: https://doi.org/10.1007/978-1-4020-8709-7_3
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