首页> 外文会议>International Soil Conservation Organization Conference vol.2; 20020526-31; Beijing(CN) >Study on Relation of Erosion and Sediment Yield in the Watershed System
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Study on Relation of Erosion and Sediment Yield in the Watershed System

机译:流域系统侵蚀与产沙量关系研究

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摘要

Based on the observation data of erosion and sediment yield in the Dalihe Watershed, a important branch of Yellow River, the conclusion is brought forward that the erosion and sediment yield in the watershed system in a long-term time can reach balance, the sediment delivery ratio is approximate equal to 1; However, a great alteration range still exist in a short-term time like a different rainfall or a particular year, the sediment delivery ratio can reach more than 1 or less than 1 because the sediment in the watershed can be delayed or be transported again by runoff erosion. Sediment delivery ratio is close with runoff deep ratio, rainfall distributing and flood peak amplitude ratio in the watershed system. The characteristics of space-time distributing of delivery ratio in the various scales watershed and the influence factors to the delivery ratio in watershed systems are illustrated and some relative models are built in this paper.
机译:根据黄河重要支流大理河流域的冲淤量观测数据,得出结论:流域系统的冲淤量在长期内可以达到平衡,输沙量大。比率大约等于1;但是,在短时间内仍存在较大的变化范围,例如降雨时间不同或特定年份,由于流域中的沉积物可能会延迟或再次被运输,因此沉积物的输送比可以达到大于1或小于1。径流侵蚀。分水岭系统中的输沙比与径流深比,降雨分布和洪峰振幅比接近。阐述了流域不同尺度下输水比的时空分布特征以及影响分水岭系统输水比的因素,建立了相关模型。

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