摘要
通过对晋祠泉域地下水动态监测资料和水文资料的分析研究,确定泉域地下水位回升的主要原因是关井压采和煤炭资源整合压采,汾河清水复流等水生态系统修复工程对泉域地下水位回升也起到了不可忽视的作用。
In this paper,the main reason of the groundwater level recovery about Jinci karst spring is analysed by groundwater dynamic monitoring data and hydrological data. The results showed that the main reason was closing wells and limiting exploitation, as well as the integration of coal resources and the reduction of coal production. In addition, the ecosystem restoration project of Fenhe river water resources on groundwater level rise also played a role can not be ignored.
出处
《山西水利科技》
2017年第1期61-63,共3页
Shanxi Hydrotechnics
关键词
晋祠泉域
岩溶地下水
关井压采
水位
回升
Jinci Spring-feeding Area
karst groundwater
closing wells
limiting exploitation
water level
rise
