| 河南省杞县地下水形成条件研究 |
| |
| 引用本文： | 黄继超,王金山,田大勇.河南省杞县地下水形成条件研究[J].地下水,2008,30(3):7-10. |
| |
| 作者姓名： | 黄继超 王金山 田大勇 |
| |
| 作者单位： | 河南省地址矿产开发局第二水文地质工程地质队,河南,郑州,450053 |
| |
| 摘 要： | 河南杞县在天然条件下，中、深层地下水的补给主要由侧向径流补给，其次为浅层地下水的越流补给。浅层地下水位高于中、深层地下水位，二者之间为薄层或透镜状粉土及粉质粘土，浅居地下水可补给中、深层水。
|
| 关 键 词： | 地下水 形成条件 河南省杞县 |
| 文章编号： | 1004-1184(2008)03-0007-03 |
| 修稿时间： | 2008年2月15日 |
Study on Formation Condition of Groundwater of Qi County in Henan Province |
| |
| HUANG Ji-chao,WANG Jin-shan,TIAN Da-yong.Study on Formation Condition of Groundwater of Qi County in Henan Province[J].Groundwater,2008,30(3):7-10. |
| |
| Authors: | HUANG Ji-chao WANG Jin-shan TIAN Da-yong |
| |
| Institution: | HUANG Ji-chao,WANG Jin-shan,TIAN Da-yong(Geology Team,No.2 Hydrogeological Engineering,Geology , Minerals Development Bureau in Henan Province,Zhenzhou 450053,China) |
| |
| Abstract: | For the natural condition,the middle and deep groundwater is mainly recharged by the side runoff,then is supplied by shallow groundwater.The water level of shallow groundwater is higher than the middle and deep groundwater level.The thin or lentoid powder and powdery clay is left between them,the shallow groundwater can replenish the middle and deep groundwater. |
| |
| Keywords: | Groundwater Formation condition Qi County in Henan Province |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
