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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 | |
| 引用本文： | 宋献方,李发东,刘昌明,唐常源,张秋英,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. |
| 作者姓名： | 宋献方 李发东 刘昌明 唐常源 张秋英 张万军 |
| 作者单位： | ( 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) |
| 基金项目： | 国家自然科学基金;中国科学院知识创新工程项目 |
| 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 |
| 文章编号： | 1000-3037（2007）03-0398-12 |
| 收稿时间： | 2006-12-31 |
| 修稿时间： | 2006-12-312007-02-26 |
Water Cycle in Taihang Mt. and Its Recharg to Groundwater in North China Plain |
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| SONG Xian-fang,LI Fa-dong,LIU Chang-ming,TANG Chang-yuan,ZHANG Qiu-ying,ZHANG Wan-jun.Water Cycle in Taihang Mt. and Its Recharg to Groundwater in North China Plain[J].Journal of Natural Resources,2007,22(3):398-408. | |
| Authors: | SONG Xian-fang LI Fa-dong LIU Chang-ming TANG Chang-yuan ZHANG Qiu-ying ZHANG Wan-jun |
| Institution: | ( 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) |
| 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 |
| Keywords: | catchment hydrology water cycle in mountainous area groundwater recharge Tai-hang Mt North China Plain |
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