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河川径流与泥沙沿程曲线
引用本文:冯光扬. 河川径流与泥沙沿程曲线[J]. 资源科学, 1993, 15(4): 13-17
作者姓名:冯光扬
作者单位:中国科学院、水利部成都山地灾害与环境研究所 成都
摘    要:研究河川径流、泥沙沿程分布规律时,本文提出的河川径流与泥沙沿程曲线法较传统的区间百分比柱状图的对比法为之简单、一目了然,是研究水资源空间分布规律的重要方法。

关 键 词:径流;输沙量;含沙量;沿程曲线;水资源;长江上游

CURVE OF THE VARIATION OF RIVER FIOW AND SEDIMENT DISCHARGE ALONG RIVER COURSE
Feng Guangyang. CURVE OF THE VARIATION OF RIVER FIOW AND SEDIMENT DISCHARGE ALONG RIVER COURSE[J]. Resources Science, 1993, 15(4): 13-17
Authors:Feng Guangyang
Abstract:The author in this paper recommends that the columnar chart contrast method which is generally used to study the distributional regulations of runoff, sediment discharge along river course should be substitited by the method of curves of river flow and sediment discharge along the river course. Curves produced from runoff difference are suit to study the runoff distributional regulations along river course Curves produced from the sediment difference are suit to study the main sources of sediment and its distributional regulations along the river course Compare to the traditional columnar chart method, this curves produced from the difference along the river course is much simpler and more obvious It is a very important method for the research of the regional and seasonal distribution of water rescurces.
Keywords:River flow  Sediment discharge  Content of Sediment  Curve produced from the difference along the river course  Water resources  Upper reach of Yangtze River  
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