Abstract
Soil erosion due to water is one of the most important land degradation processes and considered as major land degradation type in the world (UNEP 1994; Jain et al. 2010). The entire Himalayan region is facing serious problem of land degradation due to soil erosion. Deforestation and inappropriate land utilization coupled with steep sloping terrain, fragile, and young soil with erosive rainfall pattern have accelerated soil erosion in the Himalayan landscape. It reduces soil fertility by removing top soil layer and large amount of soil nutrients along with sediments (Oldeman 1994; Bai et al. 2008). It results in reduction in soil quality that adversely affects the suitability of soils for various agricultural crops and vegetation types. Harmonized statistics by ICAR (NBSS&LUP) and ISRO (NRSC) (Trivedi 2010) reported that the total area under degraded and wastelands in India is 120.72 M ha (arable land and open forest) and out of it nearly 73.27 M ha land is affected by water erosion. The average annual soil erosion rate is estimated to be 16.4 ton ha−1 year−1, resulting in an annual total soil loss of 5.3 billion tons throughout the country in India (Dhruvanarayana and Ram Babu 1983; Pandey et al. 2008). Nearly 29% of total eroded soil is permanently lost to the sea, while 61% is simply translocated from one place to another, and the remaining 10% is deposited in reservoirs.
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Kumar, S. (2019). Geospatial Approach in Modeling Soil Erosion Processes in Predicting Soil Erosion and Nutrient Loss in Hilly and Mountainous Landscape. In: Navalgund, R., Kumar, A., Nandy, S. (eds) Remote Sensing of Northwest Himalayan Ecosystems. Springer, Singapore. https://doi.org/10.1007/978-981-13-2128-3_17
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