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滹沱河径流变化分析

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通过对滹沱河流域代表站河道非汛期实测径流分析可以发现,从20世纪50年代到21世纪初,径流量减少为原来的1/3左右。非汛期上游河道来水量的减少,是造成河流下游水环境恶化的根本原因。大规模人类活动使流域下垫面情况发生了变异,使近年来同量级年降水条件下,天然年径流减少超过四成,而同时用水量占来水量的比例却在逐年增加,导致下游河道常年断流干涸,水环境严重恶化。以南水北调中线建成供水为契机,重新确立水库调度中防洪、供水和下游河流水环境保护的关系,是恢复河流水环境的必要途径。
Variation of runoff in Hutuo River
Based on the analysis of the runoff observations from t he representative stations during the non-flood season, runoff in the H utuo River in the early 2000s has decreased to one t hird of that in 1950s. The decreasing of the incoming w ater from the upstream during the non-flood season is the main reason causing the serious environmental deterioration in the low er reaches. Large-scale human activities have changed the underlying surface conditions of the H utuo River Basin. As a result, the natural annual runoff has decreased by more t han 40% under the same level of the annual precipitat ion in recent years. M eanw hile, the percentage of the w at er consumpt ion in the total w ater is increasing yearly, w hich leads to that the river drying-up becomes nor-mal and the w ater environment is det eriorating seriously in the lower reaches of the Hutuo River. The M iddle Route of the Sout h-t o-North Water Diversion Project is an opportunity to re-establish t he relationships betw een flood cont rol, w ater supply, and environment protect ion in the lower reaches, and then to restore the w ater environment of the H utuo River.

H utuo Riverrunoffw ater environmentw ater consumption

程双虎、王海宁、刘佳

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河北省水文水资源勘测局,石家庄 050031

中国水利水电科学研究院 流域水循环模拟与调控国家重点实验室,北京 100038

滹沱河 径流量 水环境 用水量

国家自然科学基金人力资源和社会保障部留学人员科技活动择优资助项目流域水循环模拟与调控国家重点实验室(中国水利水电科学研究院)人才培育课题

51209225WR0135A0320142014RC06

2014

南水北调与水利科技(中英文)
河北省水利科学研究院

南水北调与水利科技(中英文)

CSTPCDCSCD北大核心
影响因子:0.772
ISSN:2096-8086
年,卷(期):2014.(5)
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