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河川径流与泥沙沿程曲线

CURVE OF THE VARIATION OF RIVER FIOW AND SEDIMENT DISCHARGE ALONG RIVER COURSE
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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气泥沙沿程曲线法较传统的区间百分比柱状图对比法为之简单、一目了然,是研究水资源空间分布规律的重要方法。 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.
作者 冯光扬
机构地区 中国科学院
出处 《自然资源》 CSCD 北大核心 1993年第4期13-17,共5页
关键词 径流 输沙量 水资源 泥沙 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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参考文献2

  • 1顾恒岳,长江三峡工程对生态与环境影响及其对策研究论文集,1987年
  • 2团体著者,川西滇北地区水文地理,1985年

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