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黄土高原典型流域次降雨径流侵蚀产沙规律研究
引用本文:侯建才,李占斌,崔灵周.黄土高原典型流域次降雨径流侵蚀产沙规律研究[J].西北农林科技大学学报(社会科学版),2008,36(2):210-214.
作者姓名:侯建才  李占斌  崔灵周
作者单位:1. 河南省水利厅,河南,郑州,450003;西安理工大学,水利水电学院,陕西,西安,710048
2. 西安理工大学,水利水电学院,陕西,西安,710048;中国科学院,水利部,水土保持研究所黄土高原土壤侵蚀与旱地农业国家重点实验室,陕西,杨凌,7121004
3. 温州大学,生命与环境科学学院,浙江,温州,325027
4. 西安理工大学,水利水电学院,陕西,西安,710048
基金项目:国家自然科学基金 , 中国博士后科学基金
摘    要:【目的】研究黄土高原地区小流域次降雨径流侵蚀产沙规律,建立适宜于该地区的侵蚀产沙预报模型。【方法】根据岔巴沟流域32年实测的水沙资料,采用径流侵蚀功率、地貌分形信息维数的计算模型及多元非线性回归方法,分析了黄土高原地区岔巴沟流域的次降雨径流侵蚀产沙规律。【结果】岔巴沟流域次降雨侵蚀产沙模数Ms与径流侵蚀功率E、地貌形态分形信息维数Di有很好的相关性,模型具有较高的精度和一定的适用性。【结论】基于流域径流侵蚀功率与地貌形态分形信息维数的岔巴沟流域次降雨侵蚀产沙预报模型,能够近似反映不同尺度流域次降雨径流侵蚀产沙特性及水沙传递的关系,为建立具有广泛适用性和较高预报精度的黄土高原流域次降雨径流侵蚀产沙预报模型提供了理论依据。

关 键 词:黄土高原  次降雨径流侵蚀  径流侵蚀功率  分形信息维数
文章编号:1671-9387(2008)02-020O-05
收稿时间:2007-02-24
修稿时间:2007年2月24日

Research on runoff erosion and sediment yield laws of typical watershed under single rainfall on Loess Plateau
NIE Qiang.Research on runoff erosion and sediment yield laws of typical watershed under single rainfall on Loess Plateau[J].Journal of Northwest Sci-Tech Univ of Agr and,2008,36(2):210-214.
Authors:NIE Qiang
Institution:1 Water Conservancy Bureau of Henan Province,Zhengzhou,Henan 450003,China;2 College of Water Resources and Hydroelectric Engineering,Xi’an,Shaanxi University of Technology,Xi’an,Shaanxi 710048,China;3 State Key Laboratory of Soil Erosion and Dry Farming on Loess Plateau,Institute of Soil and Water Conservation,Chinese Academy of Science and Ministry of Water Resource,Yangling,Shaanxi 712100,China;4 College of Life and Environment Sciences,Wenzhou University,Wenzhou,Zhejiang 325027,China)
Abstract:Objective] To study the laws of soil erosion and sediment yield under single rainfall runoff in small watershed on Loess Plateau, the soil erosion and sediment yield prediction model adapted to this region was established. Method] Adopted runoff erosion power model and topographical fractal information dimension model on basis of observed data of runoff and sediment in Chabagou watershed for 32 years, the sediment yield laws under single rainfall runoff was analyzed through applying multielement nonlinear regression method. Result] The result showed that there was close relation between sediment yield modulus M, and runoff erosion power E, topographical fractal information dimension Di, the model had good precision and definite applicability. Conclusion] Based on runoff erosion power, geomorphological features and topographical fractal information dimension,the forecast model for runoff erosion in Chabagou watershed under single rainfall can roughly reflect the characteristics and its relationship with water and sediment power. This research will provide theoretical basis to establish watershed runoff erosion and sediment yield predictive model which had comprehensive applicability and preferable prediction precision on Loess Plateau.
Keywords:Loess Plateau  runoff erosion under single rainfall  runoff erosion power  topographical
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