摘要
以衡水市水文地质普查报告和衡水市地下水资源开发利用规划等相关资料为基础,说明了研究地区的水文地质条件,采用水均衡原理,对衡水市浅层地下水水量进行了分析计算,计算结果表明:衡水市地下水补排均衡差符合相关要求,主要补给源为降水入渗,主要排泄量为人工开采量和越流排泄量。
Together with the hydrogeologic conditions reported in Hengshui census for hydrogeology and groundwater exploitation and utilization plan, the paper analyzes the balance of groundwater flow. The result indicates that groundwater recharge almost equals to groundwater drainage. The main recharge source is precipitation which slowly seep into earth, and groundwater in the studied area is drains out mainly by exploitation and leakage.
出处
《地下水》
2013年第5期24-25,31,共3页
Ground water
关键词
衡水市
地下水
水量均衡
Hengshui City, groundwater and water balance