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ISSN: 2333-9721
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资源科学  1993 

CURVE OF THE VARIATION OF RIVER FIOW AND SEDIMENT DISCHARGE ALONG RIVER COURSE
河川径流与泥沙沿程曲线

Keywords: River flow,Sediment discharge,Content of Sediment,Curve produced from the difference along the river course,Water resources,Upper reach of Yangtze River
径流
,输沙量,含沙量,沿程曲线,水资源,长江上游

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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.

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