摘要
根据河北省近年来地下水水位实际监测数据,结合降水量、蒸发量等影响控制因素,分析了河北省不同区域不同含水层系统内16种主要的地下水动态类型。得出河北省坝上高原及河北平原浅层地下水、岩溶泉域地下水以及基岩裂隙水补给源以降水入渗补给为主,坝上高原深层地下水、山间盆地地下水补给源以侧向补给为主,河北平原深层地下水补给源为径流、越流补给。排泄方式以开采为主,蒸发、泉群排泄次之。
Groundwater in Hebei province were classified into 16 dynamic types based on monitoring data such as precipitation,evaporation. Precipitation was the main recharge method of for groundwater in Hebei Bashang plateau,shallow groundwater in Hebei plain,karst water and bedrock fissure water,lateral recharge was the main recharge method of groundwater in intermountain basins and deep groundwater in Hebei Bashang plateau,runoff and leaky are the main method of deep groundwater Hebei plain. Exploitation was the main discharge method,evaporation and spring are less.
作者
栗学梅
Li Xuemei(Hydrogeology and Engineering Geology Survey Institute of Hebei Province,Shijiazhuang 050000,China)
出处
《山西建筑》
2018年第17期216-217,共2页
Shanxi Architecture
关键词
地下水
动态类型
降水量
蒸发量
groundwater
dynamic type
preclpitation
evaporation
