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Effects of Vegetation Restoration on Soil Erosion on the Loess Plateau: A Case Study in the Ansai Watershed

机译:植被恢复对黄土高原土壤侵蚀的影响 - 以安西分水岭为例

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摘要

Large-scale vegetation restoration greatly changed the soil erosion environment in the Loess Plateau since the implementation of the “Grain for Green Project” (GGP) in 1999. Evaluating the effects of vegetation restoration on soil erosion is significant to local soil and water conservation and vegetation construction. Taking the Ansai Watershed as the case area, this study calculated the soil erosion modulus from 2000 to 2015 under the initial and current scenarios of vegetation restoration, using the Chinese Soil Loess Equation (CSLE), based on rainfall and soil data, remote sensing images and socio-economic data. The effect of vegetation restoration on soil erosion was evaluated by comparing the average annual soil erosion modulus under two scenarios among 16 years. The results showed: (1) vegetation restoration significantly changed the local land use, characterized by the conversion of farmland to grassland, arboreal land, and shrub land. From 2000 to 2015, the area of arboreal land, shrub land, and grassland increased from 19.46 km2, 19.43 km2, and 719.49 km2 to 99.26 km2, 75.97 km2, and 1084.24 km2; while the farmland area decreased from 547.90 km2 to 34.35 km2; (2) the average annual soil erosion modulus from 2000 to 2015 under the initial and current scenarios of vegetation restoration was 114.44 t/(hm²·a) and 78.42 t/(hm²·a), respectively, with an average annual reduction of 4.81 × 106 t of soil erosion amount thanks to the vegetation restoration; (3) the dominant soil erosion intensity changed from “severe and light erosion” to “moderate and light erosion”, vegetation restoration greatly improved the soil erosion environment in the study area; (4) areas with increased erosion and decreased erosion were alternately distributed, accounting for 48% and 52% of the total land area, and mainly distributed in the northwest and southeast of the watershed, respectively. Irrational land use changes in local areas (such as the conversion of farmland and grassland into construction land, etc.) and the ineffective implementation of vegetation restoration are the main reasons leading to the existence of areas with increased erosion.
机译:大规模的植被恢复大大1999年以来,“退耕还林工程”(GGP)的实施改变了土壤侵蚀环境黄土高原评估土壤侵蚀植被恢复的影响是当地的土壤和水的保护和显著植被建设。取安塞流域视情况面积,本研究计算从2000年土壤侵蚀模数到2015植被恢复的初始和当前情景下,使用中国土壤黄土等式(CSLE),基于降雨和土壤数据,遥感图像和社会经济数据。土壤侵蚀植被恢复的作用下,通过两个场景,年均土壤侵蚀模16的年际间来进行评价。结果表明:(1)植被恢复显著改变当地土地使用,其特征在于通过向农田草地,土地树栖和灌木地转换。从2000年到2015年,树栖地,灌木林地面积,草场从19.46平方公里增加,19.43平方公里和719.49平方公里到99.26平方公里,75.97平方公里和1084.24平方公里;而耕地面积从547.90平方公里降至34.35平方公里; (2)从2000年平均土壤侵蚀模数,以2015植被恢复的初始和当前情景下是114.44吨/(hm²·a)和78.42吨/(hm²·a)中,分别与平均每年减少4.81 ×106吨得益于植被恢复土壤侵蚀量的; (3)占主导地位的土壤侵蚀强度从“严重和光的侵蚀”到“中度和轻度糜烂”,植被恢复大大改善在研究区域中的土壤侵蚀环境改变; (4)区域具有增加的侵蚀及减少侵蚀交替分布的,占48%,总面积的52%,并分别主要分布在流域的西北和东南,。在局部地区不合理的土地利用变化(如农田,草场转为建设用地等的转换)以及执行不力植被恢复是导致的增加的水土流失面积存在的主要原因。

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