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首页> 外文期刊>Natural Hazards >Modelling of stream run-off and sediment output for erosion hazard assessment in Lesser Himalaya: need for sustainable land use plan using remote sensing and GIS: a case study
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Modelling of stream run-off and sediment output for erosion hazard assessment in Lesser Himalaya: need for sustainable land use plan using remote sensing and GIS: a case study

机译:小径喜马拉雅山河流径流和沉积物输出模型用于侵蚀危害评估:需要使用遥感和GIS进行可持续土地利用计划:一个案例研究

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Assessment and inventory on soil erosion hazard are essential for the formulation of successful hazard mitigation plans and sustainable development. The objective of this study was to assess and map soil erosion hazard in Lesser Himalaya with a case study. The Dabka watershed constitutes a part of the Kosi Basin in the Lesser Himalaya, India, in district Nainital has been selected for the case illustration. The average rate of erosion hazard is 0.68 mm/year or 224 tons/km2/year. Anthropogenic and geo-environmental factors have together significantly accelerated the rate of erosion. This reconnaissance study estimates the erosion rate over the period of 3 years (2006–2008) as 1.21 mm/year (398 tons/km2/year) in the barren land having geological background of diamictite, siltstone and shale rocks, 0.92 mm/year (302 tons/km2/year) in the agricultural land with lithology of diamictite, slates, siltstone, limestone rocks, while in the forest land, it varies between 0.20 mm/year (66 tons/km2/year) under dense forest land having the geology of quartzwacke and quartrenite rocks and 0.40 mm/year (132 tons/km2/year) under open forest/shrubs land having geological setup of shale, dolomite and gypsum rocks. Compared to the intensity of erosion in the least disturbed dense forest, the erosion rate is about 5–6 times higher in the most disturbed agricultural land and barren land, respectively. The erosion hazard zones delineated following scalogram modelling approach. Integrated scalogram modelling approach resulted in severe classes of soil erosion hazard in the study area with numerical values of Erosion Hazard Index (EHI) ranging between 01 (very low hazard) and 5 (very high hazard).
机译:对土壤侵蚀危害的评估和清单对于制定成功的危害缓解计划和可持续发展至关重要。这项研究的目的是通过案例研究评估和绘制小喜马拉雅山的土壤侵蚀危害。达比卡流域构成了印度小喜马拉雅山Kosi盆地的一部分,该案例被选为奈尼塔尔地区。平均侵蚀危害率为0.68 mm /年或224吨/ km 2 /年。人为和地球环境因素共同大大加速了侵蚀速度。这项侦查研究估计,在具有铁矾土,粉砂岩地质背景的贫瘠土地上,三年(2006-2008年)的侵蚀速率为1.21毫米/年(398吨/公里 2 /年)在土壤中,铁素体,板岩,粉砂岩,石灰岩的岩性为0.92 mm /年(302吨/ km 2 /年),而林地则为0.20在具有石英瓦克和方石英岩石地质的茂密林地下,毫米/年(66吨/公里 2 /年)/0.40毫米/年(132吨/公里 2 /年)在具有页岩,白云石和石膏岩石地质构造的开阔森林/灌木丛土地上。与受干扰最少的茂密森林中的侵蚀强度相比,受干扰最大的农田和贫瘠土地的侵蚀率分别高出约5-6倍。按照比例尺建模方法划定了侵蚀危险区。集成的比例尺建模方法在研究区域导致了严重的土壤侵蚀危害类别,其侵蚀危害指数(EHI)的数值介于01(非常低的危害)到5(非常高的危害)之间。

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