The breakdown of solid rock into smaller particles and its removal by wind. It may occur on any soil whose surface is dry, unprotected by vegetation (to bind it at root level and shelter the surface) and consists of light particles. The mechanisms include straightforward picking up of dust and soil particles by the airflow and the dislodging or abrasion of surface material by the impact of particles already airborne. (Source: ALL)



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Displaying results 1 - 17 of 17 record(s) tagged with this keywordClick/tap on any title to see full details of the record
Sweeting MM, Lancaster N 1982. Solutional and wind erosion forms on limestone in the central Namib Desert. Zeitschrift für Geomorphologie 26 (2) 197-207
Gehring AU, Riahi N, Kind J, Almqvist BSG, Weidler PG 2014. The formation of the Namib Sand Sea inferred from the spatial pattern of magnetic rock fragments. Earth and Planetary Science Letters 395 168-172
Zobeck TM 1991. Soil properties affecting wind erosion. Journal of Soil and Water Conservation 46 (2) 112-118
Codilean AT, Bishop P, Stuart FM, Hoey TB, Fabel D, Freeman SPHT 2007. Single-grain cosmogenic 21Ne concentrations in fluvial sediments reveal spatially variable erosion rates. Geology 36 (2) 159-162
Goliger AM, Retief JV 2007. Severe wind phenomena in Southern Africa and the related damage. Journal of Wind Engineering and Industrial Aerodynamics 95 (9 - 11) 1065 - 1078
Strohbach BJ 2000. Soil erosion - causative factors, extent and prevention. Agri-Info 6 (1) 8-14
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Soil erosion_causative factors_extent and prevention.pdf 607.17 KB
Strohbach B 2000. Soil erosion - causitive factors, extent and prevention. Agri-Info 6 (1) 8-14
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AgriInfo6_1_2000_Soil erosion.pdf 616.46 KB