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Changes in soil erosion and sediment transport based on the RUSLE model in Zhifanggou watershed, China

机译:基于Zhifanggou流域的破坏模型的土壤侵蚀与沉积物运输的变化

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In this paper, changes of sediment yield and sediment transport were assessed using the Revised Universal Soil Loss Equation (RUSLE) and Geographical Information Systems (GIS). This model was based on the integrated use of precipitation data, Landsat images in 2000, 2005 and 2010, terrain parameters (slope gradient and slope length) and soil composition in Zhifanggou watershed, Gansu Province, Northwestern China. The obtained results were basically consistent with the measured values. The results showed that the mean modulus of soil erosion is 1224, 1118 and 875 tkm~(-2) yr~(-1) and annual soil loss is 23 130, 21 130 and 16536 in 2000, 2005 and 2010 respectively. The measured mean erosion modulus were 1581 and 1377 tkm~(-2) yr~(-1), and the measured annual soil loss were 29 872 and 26 0221 in 2000 and 2005. From 2000 to 2010, the amount of soil erosion was reduced yearly. Very low erosion and low erosion dominated the soil loss status in the three periods, and moderate erosion followed. The zones classified as very low erosion were increasing, whereas the zones with low or moderate erosion were decreasing. In 2010, no zones were classified as high or very high soil erosion.
机译:在本文中,产沙输沙的变化使用经修订的通用土壤流失方程(RUSLE)和地理信息系统(GIS)进行了评估。这种模式是基于在2000年,2005年和2010年的综合运用降水资料,陆地卫星影像,地形参数(坡度和坡长),并在纸坊土壤成分分水岭,甘肃省,中国西北地区。将所得到的结果与测量值基本一致。结果表明,土壤侵蚀模数平均值是1224,1118和875吨公里〜(-2)年〜(-1),年土壤流失23 130 21 130和16536于2000年,2005年分别和2010年。测得的平均侵蚀模数分别为1581和1377 TKM〜(-2)年〜(-1),和测量的年土壤流失进行29 872和于2000年26 0221和2005从2000年到2010年,土壤侵蚀的量为每年减少。极低的侵蚀和冲刷低主导了三个时期的水土流失状况,中度糜烂紧随其后。列为非常低侵蚀的区域都在增加,而具有低或中度糜烂下降的区域。在2010年,没有区被列为高或非常高的水土流失。

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