摘要
内陆地区地下水咸化有别于海水入侵,以焦作市为例,利用不同水体的稳定同位素(如O18和H2)和水化学组成,判定地下水咸化来源。结果发现,焦作市深层地下水氯化物浓度升高与工业废水有关,工业废水借助断层破碎带对研究区深层地下水(D8)产生影响;焦作市浅层地下水氯化物浓度升高与工业废水和生活污水的混合水有关,混合水透过河床底部包气带进入浅层地下水对其产生影响。泉水、农业面源和大气降水不是研究区地下水氯化物污染的来源。
Inland groundwater salinization was different from seawater intrusion,and in Jiaozuo City,stable isotopic（e.g.O18and H2） and hydrochemical compositions of different water bodies were introduced to determine groundwater salinization sources.Results indicated that chloride pollution in deep groundwater was connected with industrial waste water which found its way into groundwater（D8） through faults and fractures,and chloride pollution of shallow groundwater was related with sewage which was mixed with industrial waste water,and then infiltrated into shallow groundwater through the unsaturation zone.Spring water,agriculture non-point source and local precipitation had no influence on chloride pollution of local groundwater.
出处
《地球与环境》
CAS
CSCD
北大核心
2010年第2期177-183,共7页
Earth and Environment
基金
河南省教育厅自然科学基金项目<同位素分析应用于追踪地下水污染源研究的理论基础>
项目编号:2004923004
关键词
稳定同位素
水化学
地下水咸化
焦作市
stable isotope
hydrochemistry
groundwater salinization
Jiaozuo City
作者简介
张东（1978-），男，博士研究生，主要从事地下水污染环境地球化学研究，E-mail：zhangdong@hpu．edu．cn
