JOURNAL OF YANGTZE RIVER SCIENTIFIC RESEARCH INSTI ›› 2013, Vol. 30 ›› Issue (5): 22-26.DOI: 10.3969/j.issn.1001-5485.2013.05.06

• Watre-Soil conservation and ECO-Construction • Previous Articles     Next Articles

Rapid Estimation of Soil Erosion Amount in Small Watershed Based on Standards for Soil Erosion Gradation:An Example from Bijie Monitoring Station in Chishuihe River Basin

WANG Zhi-gang1,2,TU Ren-meng3,SUN Jia-jia1,2,HU Bo1,2,DING Wen-feng1,2,XU Wen-yu1,ZHANG Ping-cang1,2   

  1. 1. Soil and Water Conservation Department, Yangtze River Scientific Research Institute, 430010, China; 2. Hubei Key Laboratory of Water Resources & Eco-environiment, Yangtze River Scientific Research Institute, Wuhan 430010, China; 3.Institute of Economy, Hubei Academy of Social Sciences, Wuhan 430077,China
  • Received:2012-10-11 Revised:2013-04-28 Online:2013-04-28 Published:2013-04-28

Abstract: Even for simple empirical model,it is difficult to obtain enough basic data of soil erosion. Establishing a simpler model for soil erosion amount estimation is necessary. Land use types,surface slopes,and vegetation coverage in Maojiaowan small watershed in Chishuihe River Basin were surveyed,and the soil erosion amount was estimated according to the method in Standards for Classification and Gradation of Soil Erosion. In order to accurately estimate the soil erosion modulus in the karst regions of Southwest China,the standards for gradation of hydraulic erosion in Standards for Classification and Gradation of Soil Erosion were revised. Additionally,it is necessary to use more accurate methods to measure vegetation coverage. It’s also pointed out that the soil erosion spatial distribution was controlled by landform in the karst regions of Southwest China,and it is necessary to conduct further study on the spatial distribution patterns of soil erosion to reveal the effect of landform on soil erosion.

Key words: gradation of soil erosion , small watersheds , soil erosion amount , Chishuihe River Basin , Three Gorges Project

CLC Number: 

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