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Evaluation of soil loss change after Grain for Green Project in the Loss Plateau: a case study of Yulin, China

机译:高原干旱区退耕还林还草后土壤流失变化评价-以榆林市为例

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Soil erosion is one of the serious and urgent issues in the Loss Plateau of China. Chinese government has implemented Grain for Green Project to restore the ecological environment since 1999. In order to explore the spatiotemporal evolution of erosion and sediment yield before and after Grain for Green Project in the Loss Plateau, annual soil loss of Yulin from 2000 to 2013 is estimated by Chinese Water Erosion on Hillslope Prediction Model in conjunction with Remote Sensing and Geographic Information Systems. This model has the characteristics of a simple algorithm and can be applied to predict erosion in the Loss Plateau. The result shows that vegetation cover increased significantly after Grain for Green Project, and the annual average value of NDVI increased from 0.20 to 0.33. The spatiotemporal variations of soil erosion are largely related to rainfall erosion distribution, slope, and land use type. The overall soil erosion categories in the south region are higher than those of the northwest. Mid slopes and valleys are the major topographic contributors to soil erosion. With the growth of slope gradient, soil erosion significantly increased. The soil loss has a decreasing tendency after Grain for Green Project. Although the rainfall of 2002 and 2013 is similar, the soil loss decreased from 5192.86 to 3598.94 t/(km(2)a), decreasing by 30.33%. It is also expressed that soil loss appears a reducing trend in the same degree of slope and elevation in 2002, 2007, and 2013. Under the simulation of the maximum and the minimum rainfall, soil erosion amount in 2013 decreased by 29.16 and 30.88%. The study proved that GFG has already achieved conservation of water and soil. The results indicate that the vegetation restoration as part of the Grain for Green Project on the Loss Plateau is effective.
机译:在中国的高原地区,水土流失是严重而紧迫的问题之一。自1999年以来,中国政府实施了“退耕还林工程”以恢复生态环境。为探讨失水高原退耕还林工程前后侵蚀和沉积物产量的时空演变,榆林市2000年至2013年的年土壤损失为结合遥感和地理信息系统,由中国水蚀坡度预测模型估算。该模型具有简单算法的特征,可用于预测损失高原的侵蚀。结果表明,退耕还林后植被覆盖度显着增加,NDVI的年均值从0.20增加到0.33。土壤侵蚀的时空变化主要与降雨侵蚀分布,坡度和土地利用类型有关。南部地区的总体土壤侵蚀类别高于西北地区。中坡和山谷是造成土壤侵蚀的主要地形因素。随着坡度的增大,水土流失明显增加。退耕还林工程后,水土流失呈下降趋势。尽管2002年和2013年的降雨量相似,但土壤流失量从5192.86吨减少至3598.94吨/(km(2)a),下降了30.33%。还表明,在2002年,2007年和2013年相同的坡度和海拔高度下,水土流失呈减少趋势。在最大和最小降雨的模拟下,2013年的土壤侵蚀量分别减少了29.16和30.88%。研究证明,GFG已经实现了水土保持。结果表明,作为高原地区退耕还林工程的一部分,植被恢复是有效的。

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