地下水水源地脆弱性评价研究  

Research on the Assessment of Groundwater Source Vulnerability

作　　者：王丽红[1] 王开章[2] 李晓[3] 焦玉国 

机构地区：[1]山东农业大学资源与环境学院,山东泰安271018 [2]山东农业大学水利土木工程学院,山东泰安271018 [3]山东省水利科学研究院,山东济南250013 [4]山东省地质矿产勘查开发局第五地质大队,山东泰安271021

出　　处：《中国农村水利水电》2008年第11期22-25,共4页China Rural Water and Hydropower

基　　金：国家科技支撑计划子课题(2006BAD01B08-01)

摘　　要：从水源地的水文地质结构抵御外界污染的能力出发,利用地下水GMS模拟系统和东武水源地钻孔资料,实现了水源地水文地质结构实体的可视化;在此基础上,运用DRAMIC模型对水源地进行了脆弱性评价。研究结果表明,该水源地的两个含水层(孔隙水、岩溶水)为脆弱性较强,第四系孔隙水较易受到污染,岩溶水容易受到第四系孔隙水的污染。因而,应控制化肥、农药的使用,综合治理大汶河水质,保障水源地安全。The hydrological and geological structure is important to the vulnerability of the wellfield. Visualization hydrogeologicalstructure entities are established by using groundwater model software GMS together with borehole data of the Dongwu wellfield. And groundwater source vulnerability is evaluated by DRAMIC model. It indicates that the vulnerability of the water-bearing strata （pore water, karst water） are stronger, the karst water is easy to be polluted by the pore water. So chemical fertilizers and pesticides should be minimized. Furthermore, the water quality of the Dawen River should be comprehensively governed in order to protect the security of groundwater source.

关 键 词：地下水水源地 脆弱性 DRAMIC模型 GMS 

分 类 号：K523[历史地理—历史学]