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Estimation of soil erosion using RUSLE in Caijiamiao watershed, China

机译:蔡家庙流域使用RUSLE估算土壤侵蚀

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Soil erosion is a serious environmental and production problem in China. In particular, natural conditions and human impact have made the Chinese Loess Plateau particularly prone to intense soil erosion area. To decrease the risk on environmental impacts, there is an increasing demand for sound, and readily applicable techniques for soil conservation planning in this area. This work aims at the assessment of soil erosion and its spatial distribution in hilly Loess Plateau watershed (northwestern China) with a surface area of approximately 416.31 km(2). This study was conducted at the Caijiamiao watershed to determine the erosion hazard in the area and target locations for appropriate initiation of conservation measures using the revised universal soil loss equation (RUSLE). The erosion factors of RUSLE were collected and processed through a geographic information system (GIS)-based approach. The soil erosion parameters were evaluated in different ways: The R-factor map was developed from the rainfall data, the K-factor map was obtained from the soil map, the C-factor map was generated based on Landsat-5 Thematic Mapper image and spectral mixture analysis, and a digital elevation model with a spatial resolution of 25 m was derived from topographic map at the scale of 1:50,000 to develop the LS-factor map. Support practice P factor was from terraces that exist on slopes where crops are grown. By integrating the six-factor maps in GIS through pixel-based computing, the spatial distribution of soil loss in the study area was obtained by the RUSLE model. The results showed that spatial average soil erosion at the watershed was 78.78 ton ha(-1) year(-1) in 2002 and 70.58 ton ha(-1) year(-1) in 2010, while the estimated sediment yield was found to be 327.96 x 10(4) and 293.85 x 10(4) ton, respectively. Soil erosion is serious, respectively, from 15 to 35 of slope degree, elevation area from 1,126 to 1,395 m, in the particular area of soil and water loss prevention. As far as land use is concerned, soil losses are highest in barren land and those in waste grassland areas are second. The results of the study provide useful information for decision maker and planners to take appropriate land management measures in the area. It thus indicates the RUSLE-GIS model is a useful tool for evaluating and mapping soil erosion quantitatively and spatially at a river watershed scale on a cell basis in Chinese Loess Plateau and for planning of conservation practices.
机译:水土流失是中国严重的环境和生产问题。特别是自然条件和人类影响,使得中国黄土高原特别容易发生土壤侵蚀严重的地区。为了减少对环境影响的风险,对该区域的土壤保持规划提出了可靠且易于应用的可靠技术要求。这项工作旨在评估表面积约416.31 km(2)的黄土高原丘陵流域(中国西北)的土壤侵蚀及其空间分布。这项研究是在蔡家庙流域进行的,目的是使用修订后的通用土壤流失方程式(RUSLE)确定区域和目标位置的侵蚀危害,以采取适当的保护措施。 RUSLE的侵蚀因子是通过基于地理信息系统(GIS)的方法收集和处理的。以不同的方式评估土壤侵蚀参数:从降雨数据绘制R因子图,从土壤图获得K因子图,基于Landsat-5 Thematic Mapper图像生成C因子图,光谱混合分析,并从地形图以1:50,000的比例尺导出空间分辨率为25 m的数字高程模型,以开发LS因子图。支持措施的P因子来自种植农作物的山坡上的阶地。通过基于像素的计算将六因子地图集成到GIS中,通过RUSLE模型获得了研究区土壤流失的空间分布。结果表明,该流域的平均土壤侵蚀在2002年为78.78 ton ha(-1)年(-1),在2010年为70.58 ton ha(-1)年(-1),而估计的泥沙产量为分别为327.96 x 10(4)和293.85 x 10(4)吨。在特定的水土流失防治地区,水土流失严重,坡度分别为15〜35,高程区为1126〜1395m。就土地利用而言,在荒芜的土地上土壤损失最高,而在荒草地上的损失则第二。研究结果为决策者和规划者采取适当的土地管理措施提供了有用的信息。因此,它表明RUSLE-GIS模型是一种有用的工具,可以在中国黄土高原的一个流域尺度上,以单元为单位,定量和空间地评估和绘制土壤侵蚀,并规划保护措施。

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