断层的蓄水特性及对地下水的影响综述  

Water Storage Characteristics of Faults and the Effects on Groundwater

作　　者：梁丽青[1] 张瑞[1] 殷飞[1] LIANG Li-qing;ZHANG Rui;YIN Fei(Jilin Agricultural Science and Technology University, JiLin 132001, China)

机构地区：[1]吉林农业科技学院,吉林省吉林市132000

出　　处：《中小企业管理与科技》2017年第33期144-145,共2页Management & Technology of SME

基　　金：吉林农业科技学院校级青年基金项目"基于GMS的数值模拟在地下水资源评价中的应用研究"(编号:2017年213号)

摘　　要：断层是一种重要的地质构造,是地下水溶集和地下水流动的重要通道,可以形成中小型的水源地。断层蓄水构造是由断层破碎带及其节理,裂隙、孔隙、溶隙等构成了蓄水空间,具有蓄水空间相对大、富水较为不均匀、水动力条件相对较好等特点,其形成条件及其岩性等都影响着其蓄水能力和地下水流场。Fault is an important geological structure, which is an important channel for groundwater dissolution and flow. It can form small and medium water sources. The fault is composed of fault zone and its joints, cracks, porosity and so on. It has the characteristics of relatively large water storage space, relatively uneven water content and relatively good hydrodynamic conditions. Its forming conditions and its lithology and other factors al I affect its water storage capacity and groundwater flow field.

关 键 词：断层构造 蓄水性 地下水 

分 类 号：TU991.112[建筑科学—市政工程]