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黄土丘陵沟壑区中大流域侵蚀产沙模型与尺度转换研究
引用本文:蔡强国,刘纪根,郑明国. 黄土丘陵沟壑区中大流域侵蚀产沙模型与尺度转换研究[J]. 水土保持通报, 2007, 27(4): 131-135
作者姓名:蔡强国  刘纪根  郑明国
作者单位:1. 中国科学院,地理科学与资源研究所,陆地水循环及地表过程重点实验室,北京,100101
2. 长江科学院,水土保持研究所,湖北,武汉,430010
基金项目:国家自然科学基金;国家重点基础研究发展计划(973计划);中国科学院前沿领域研究基金
摘    要:由于侵蚀产沙因子时间和空间上的变异性,中大流域的侵蚀产沙过程模拟相对于小流域更为复杂化,目前已存在的物理模型和经验模型均难以很好地运用在中大流域。分析了中大流域的侵蚀产沙特点及已有的模型,认为尺度转换技术是实现大中流域侵蚀产沙模拟研究重要的途径,并对尺度转换的方法进行了探讨。

关 键 词:侵蚀产沙  中大流域  尺度  模型
文章编号:1000-288X(2007)04-0131-05
收稿时间:2007-05-20
修稿时间:2007-05-20

Sediment Yield Model and Upscaling for Medium and Large Watersheds in Hilly and Gully Region of the Loess Plateau
CAI Qiang-guo,LIU Ji-gen and ZHENG Ming-guo. Sediment Yield Model and Upscaling for Medium and Large Watersheds in Hilly and Gully Region of the Loess Plateau[J]. Bulletin of Soil and Water Conservation, 2007, 27(4): 131-135
Authors:CAI Qiang-guo  LIU Ji-gen  ZHENG Ming-guo
Affiliation:1. Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; 2. Institute of Soil and Water Conservation, Academy of Yangtze River, Wuhan , Hubei 430010, China
Abstract:Due to the spatial and temporal variations of environmental factors, the processes of soil erosion and sediment yield in medium and large watersheds are much more complex than those in small watersheds. As a result, both empirical and physics-based models can hardly be applied in medium and large watershed with a reasonable result. This paper first illustrates the characteristics of soil erosion and sediment yield in the medium and large watersheds, and then gives a review of the models developed for the watersheds. Some methodologies to upscaling, which may be an important approach to simulating the processes of soil erosion and sediment yield in the medium and large watershed, are also discussed.
Keywords:soil erosion and sediment yield   medium and large watersheds   scale   model
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