Abstract
Soil erosion is a natural process caused by water, wind, and ice that has affected the earth’s surface since the beginning of time. Soil erosion and its off-site, downstream damages are major concerns around the world (La1 1994b) causing losses in soil productivity and degradation of landscape (Walling 1983). Many of man’s activities have accelerated soil erosion (Sombroek 1995; Walling 1983). Oldeman (1994) has estimated that human-induced soil degradation has affected 15% of the world’s arable land surface. Estimates of global soil erosion rates range from 0.088 mm yr-1 (Walling 1987) to 0.30 mm yr-1 (Fournier 1960). These values led to estimates of 17.4 to 58.1 x 109 Mg of soil loss from the land surface (Walling 1990) which is carried downstream into lakes, reservoirs and estuaries where it reduces storage capacity and affects water quality, navigation, and biological productivity. On the land surface, soil erosion decreases organic matter, fine grained soil particles, water holding capacity, and rooting depth leading to loss of soil productivity and quality. The economic consequences from soil erosion on loss of productivity, land degradation, and off-site, downstream damages from eroded soil particles on water quality are a major concern. Pimentel et al. (1995) estimated the economic cost of soil erosion and subsequent sediment deposition to be $400 billion per year worldwide. While this economic estimate of the cost of erosion has been questioned (Sombroek 1995), concerns about soil loss and the estimated cost point to the need for new and improved methodologies and techniques for monitoring and quantifying soil erosion effectively and efficiently across the landscape so that effective land management practices can be applied to the land surface to control and reduce soil erosion
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Ritchie, J.C. (2000). Soil Erosion. In: Schultz, G.A., Engman, E.T. (eds) Remote Sensing in Hydrology and Water Management. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-59583-7_12
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DOI: https://doi.org/10.1007/978-3-642-59583-7_12
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