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Soil erosion assessment of a Himalayan river basin using TRMM data

机译:使用TRMM数据的喜马拉雅河流域土壤侵蚀评估

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In this study, an attempt has been made to assess the soil erosion of a Himalayan river basin, the Karnali basin, Nepal, using rainfall erosivity (R-factor) derived from satellite-based rainfall estimates (TRMM-3B42 V7). Average annual sediment yield was estimated using the well-known Universal Soil Loss Equation (USLE). The eight-year annual average rainfall erosivity factor (R) for the Karnali River basin was found to be 2620.84 MJ mm ha~(-1) h~(-1) year~(-1). Using intensity-erosivity relationships and eight years of the TRMM daily rainfall dataset (1998-2005), average annual soil erosion was also estimated for Karnali River basin. The minimum and maximum values of the rainfall erosivity factor were 1108.7 and 4868.49 MJ mm ha~(-1) h~(-1) year~(-1), respectively, during the assessment period. The average annual soil loss of the Karnali River basin was found to be 38.17 t ha~(-1) year~(-1). Finally, the basin area was categorized according to the following scale of erosion severity classes: Slight (0 to 5 t ha~(-1) year~(-1)), Moderate (5 to 10 t ha~(-1) year~(-1)), High (10 to 20 t ha~(-1) year~(-1)), Very High (20 to 40 t ha~(-1) year~(-1)), Severe (40 to 80 t ha~(-1) year~(-1)) and Very Severe (>80 t ha~(-1) year~(-1)). About 30.86% of the river basin area was found to be in the slight erosion class. The areas covered by the moderate, high, very high, severe and very severe erosion potential zones were 13.09%, 6.36%, 11.09%, 22.02% and 16.64% respectively. The study revealed that approximately 69% of the Karnali River basin needs immediate attention from a soil conservation point of view.
机译:在这项研究中,已经尝试评估喜马拉雅河流域的土壤侵蚀,尼泊尔Karnala河流域,利用衍生自卫星的降雨估计(TRMM-3B42 V7)的降雨腐蚀性(R-Factor)。利用众所周知的通用土壤损失方程(USLE)估计了平均年度沉积物产量。 Karnali River盆地的八年年平均降雨腐蚀系数(R)是2620.84 MM HA〜(-1)H〜(-1)年〜(-1)。使用强度 - 腐蚀性关系和八年的TRMM日落DataSet(1998-2005),估计卡纳里河流域的平均年度土壤侵蚀。降雨侵蚀性因子的最小值和最大值分别在评估期间分别为1108.7和4868.49 MM mm〜(-1)H〜(-1)年〜(-1)。 Karnali河流域的平均土壤流失为38.17 t ha〜(-1)年〜(-1)。最后,盆地根据以下侵蚀严重等级规模分类:轻微(0至5ta〜(-1)年〜(-1)),中等(5到10 t ha〜(-1)年〜(-1)),高(10至20ta〜(-1)年〜(-1)),非常高(20至40 t ha〜(-1)年〜(-1)),严重( 40至80 t ha〜(-1)年〜(-1)),非常严重(> 80 t ha〜(-1)年〜(-1))。发现约30.86%的河流盆地被发现是在轻微的侵蚀阶级。中等,高,非常高,严重和非常严重侵蚀潜在区域涵盖的区域分别为13.09%,6.36%,11.09%,22.02%和16.64%。该研究表明,大约69%的卡纳里河流域需要从土壤守恒的角度立即关注。

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