山东省烟台市牟平区水文地质特征分析  

Analysis of hydrogeological characteristics in shandong Yantai District

作　　者：高松 扈胜涛 白莹 GAO Song;HU Sheng-tao;BAI Ying(the third institute of geology and mineral exploration of shandong province,yantai 264004,China)

机构地区：[1]山东省第三地质矿产勘查院,山东烟台264004

出　　处：《地下水》2020年第3期115-119,共5页Ground water

基　　金：山东省半岛蓝色经济区1:10万区域水文地质工程地质环境地质综合调查报告(牟平幅J51D008004)。

摘　　要：通过前期资料收集、水文地质调查、水文地质钻探、水文地质试验、地下水水位测量等手段,查明了牟平区水文地质条件,从而为牟平区地下水环境保护及水资源开发利用提供借鉴意义。调查结果表明,牟平区所处水文地质单元为鲁东低山丘陵松散岩碎屑岩变质岩类水文地质区(Ⅲ)、胶北隆起北坡水文地质亚区(Ⅲ2)、威海低山丘陵裂隙水水文地质小区(Ⅲ2-3);地下水可划分为四大类型:第四系松散岩类孔隙含水岩组(Ⅰ)、碎屑岩类孔隙裂隙含水岩组(Ⅱ)、碳酸盐岩类岩溶裂隙含水岩组(Ⅲ)及基岩裂隙含水岩组(Ⅳ)。Get through the previous data collection,hydrogeological survey,hydrogeological drilling,hydrogeological test,groundwater level measurement and other means,the hydrogeological conditions of shandongdistrict will be investigated.The survey results are of great significance to the groundwater environmental protection and water resources development and utilization of shandong district.The survey results indicate that the hydrogeological unit of shandong district is the Hydrogeological area of Loose rock,clastic rock and metamorphic rock in low mountains and hills of Ludong(Ⅲ),hydrogeological sub area of the north slope of Jiaobei uplift(Ⅲ2),fissure water hydrogeological community in low mountains and hills of Weihai(Ⅲ2-3).And groundwater in this area can be divided into four types:Quaternary loose rock pore water bearing formation(Ⅰ),Clastic rock pore fissure water bearing formation(Ⅱ),Carbonate karst fissure water bearing formation(Ⅲ)and bedrock fissure water bearing formation(Ⅳ).

关 键 词：含水岩组 水文地质 牟平区 烟台市 

分 类 号：P641.6[天文地球—地质矿产勘探]