太行山区水循环及其对华北平原地下水补给的研究

doi:10.11849/zrzyxb.2007.03.009

自然资源学报 ›› 2007, Vol. 22 ›› Issue (3): 398-408.doi: 10.11849/zrzyxb.2007.03.009

太行山区水循环及其对华北平原地下水补给的研究

宋献方李发东刘昌明唐常源张万军

( 1.中国科学院地理科学与资源研究所陆地水循环及地表过程重点实验室, 北京100101; 2.千叶大学,
日本千叶263- 8522; 3.中国科学院遗传与发育生物学研究所农业资源研究中心, 石家庄050021)

收稿日期:2007-02-03 修回日期:2007-03-03 出版日期:2007-05-15 发布日期:2007-05-15
通讯作者: 宋献方( 1965- ) , 男, 研究员, 博士生导师, 主要研究方向为流域水循环与水环境、环境同位素水文学。 E-mail:E-mail: songxf@igsnrr.ac.cn
作者简介:宋献方( 1965- ) , 男, 研究员, 博士生导师, 主要研究方向为流域水循环与水环境、环境同位素水文学。
基金资助:
国家自然科学基金项目(40671034)和中国科学院知识创新工程重要方向项目(KZCX3-SW-428) 共同资助。

Water Cycle in Taihang Mt. and Its Recharg to Groundwater in Nor th China Plain

SONG Xian-fang1, LI Fa-dong2, 3, LIU Chang-ming1, TANG Chang-yuan1, 2, ZHANG Qiu-ying2, ZHANG Wan-jun3

( 1.Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences
and Natural Resources Research, CAS, Beijing 100101, China; 2.Chiba University, Chiba
263- 8522, Japan; 3.Center for Agricultural Resources Research, Institute of
Genetics and Developmental Biology, CAS, Shijiazhuang 050021, China)

Received:2007-02-03 Revised:2007-03-03 Online:2007-05-15 Published:2007-05-15

摘要/Abstract

摘要： 山区水循环研究不仅对山区本身, 对与其相连的山前平原地下水的补给也具有重要意义。太行山区作为华北平原的重要水源补给区, 其水循环现状以及对华北平原地下水的补给研究尚少, 许多机理还不明确。研究通过阐述山区水循环过程与机理, 结合地处太行山中段的牛家庄实验流域的实例研究, 对太行山区对华北平原地下水的补给过程进行了分析。2004 年4—11 月的研究结果表明, 牛家庄流域对山前的侧向补给量为1.53×106m3, 补给系数(补给总量/降水总量)为0.242。流域的下游补给系数最大, 中游次之, 上游最小。最后, 用概念模型对太行山区流域水循环机制和山前侧向补给的机理进行了阐述。

关键词: 流域水文, 山区水循环, 地下水补给, 太行山, 华北平原

Abstract: Researches on water cycle in Taihang Mt. is vital not only to mountainous areas but also to groundwater recharge in adjacent piedmont.As one of the essential recharge sources for North China Plain (NCP) , a few results on status of water cycle and groundwater recharge into NCP have been reported, and the associated mechanisms have not been revealed clearly.Here, the mechanism and recharge processes of water in Taihang Mt. to NCP, with a case study in Niujiazhuang Catchment and the nested Shimen Catchment within it which is located at the middle of Taihang Mt., were presented.The results, from April to November 2004 for example, indicate the amount of lateral recharge from mountainous area to the adjacent piedmont was 1.53×106m3 with recharge ratio ( calculated by total recharge /total precipitation) of 0.242 in the order of upper reaches

Key words: catchment hydrology, water cycle in mountainous area, groundwater recharge, Taihang
Mt., North China Plain

中图分类号:

P339

宋献方李发东刘昌明唐常源张万军
. 太行山区水循环及其对华北平原地下水补给的研究[J]. 自然资源学报, 2007, 22(3): 398-408.

SONG Xian-fang1, LI Fa-dong2, 3, LIU Chang-ming1, TANG Chang-yuan1, 2,. Water Cycle in Taihang Mt. and Its Recharg to Groundwater in Nor th China Plain[J]. JOURNAL OF NATURAL RESOURCES, 2007, 22(3): 398-408.

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太行山区水循环及其对华北平原地下水补给的研究

Water Cycle in Taihang Mt. and Its Recharg to Groundwater in Nor th China Plain

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