Estimation of soil erosion using RUSLE in Caijiamiao watershed, China
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- 作者：Jinghu Pan (1)
Yan Wen (1) - 关键词：Soil erosion ; RUSLE ; Remote sensing ; GIS ; Caijiamiao watershed
- 刊名：Natural Hazards
- 出版年：2014
- 出版时间：April 2014
- 年：2014
- 卷：71
- 期：3
- 页码：2187-2205
- 全文大小：2,144 KB
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Yan Wen (1)
1. College of Geographic and Environmental Science, Northwest Normal University, 967 Anning East Road, Lanzhou, 730070, People’s Republic of China - ISSN：1573-0840
文摘
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?km2. 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??year? in 2002 and 70.58?ton?ha??year? in 2010, while the estimated sediment yield was found to be 327.96?×?104 and 293.85?×?104?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.