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锦江水库对下游径流年内分配影响分析

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基于锦江流域仁化、长坝两个研究站点及参照站点犁市1958~2009年的日径流资料,采用集中度、集中期、不均匀系数与极值比4项指标定量研究了各站点径流年内分配的规律,并着重比较分析了仁化、长坝两站在锦江水库建库前后的径流年内分配情况.结果表明:控制时段取5d时,犁市站径流集中度与集中期、不均匀系数和极值比均呈上升趋势,年内径流分配趋于不均匀;而仁化站与长坝站径流集中度和不均匀系数都呈下降趋势,年内径流分配趋于均匀.控制时段取一个月时,犁市站径流极值比有微弱下降趋势,而仁化站径流极值比上升趋势明显.总体而言,锦江水库运行后使得下游径流年内分配趋于均匀化,但锦江下游径流的变化幅度增大.
Analysis of Effect of Jinjiang Reservoir on Downstream Annual Streamflow Distribution
Based on the daily flow at Renhua,Changba and Lishi stations covering 1958-2009,statistical analysis was done on the concentration degree,concentration period,nonuniform coefficient and extrema ratio with aim to understand the annual distribution of streamflow,and mainly analyzed the streamflow of Renhua and Changba before and after Jinjiang reservoir used.The results show that the concentration degree,the concentration period,the nonuniform coefficient and the extrema ratio of Lishi were on the rise when studied time was five days,which indicated that the annual streamflow distribution is becoming nununiform.The concentration degree and the nonuniform coefficient of Renhua and Changba were on the downward trend,which indicated that the annual streamflow distribution is becoming uniform.Studied time was one month,the extrema ratio of Lishi had a weak downward trend; and the rise trend of Renhua's extrema ratio was obvious.In general,the downstream annual streamflow distribution was more uniform after Jinjiang reservoir used; but the extrema ratio was increased than before.

Jinjiang reservoirannual streamflow distributionconcentration degreeconcentration periodnonuniform coefficientextrema ratio

陈伟东

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河海大学 水文水资源学院,南京 210098

锦江水库 径流年内分配 集中度 集中期 不均匀系数 极值比

水利部公益性行业科研专项项目

201501059

2016

三峡大学学报(自然科学版)
三峡大学

三峡大学学报(自然科学版)

CSTPCD
影响因子:0.401
ISSN:1672-948X
年,卷(期):2016.38(2)
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