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环境水文地质研究中的C1~-示踪法
引用本文:邱汉学,刘贯群,史致丽,李铁,祝陈坚.环境水文地质研究中的C1~-示踪法[J].中国海洋大学学报(自然科学版),1996(1).
作者姓名:邱汉学  刘贯群  史致丽  李铁  祝陈坚
作者单位:College of Marine Geosciences,Chemistry Department
摘    要:用CI一分析法可确定地下水污染途径,分析污染强度、海水入侵范围与程度、水动力场特征等问题。通过实验证实包气带中CI不易被吸附,不参与化学反应,包气带及地下水中极易迁移,形成天然的和人工的地下水运动示踪剂。

关 键 词:环境水文地质  C1~-迁移性质  C1~-示踪法  水动力场分析  污染途径分析  海水入侵  范围判别

C1~- TRACING METHOD IN ENVIRONMENTAL HYDROGEOLOGY
Qiu Hanxue, Liu Guanqun, Shi Zhili, Li Tie, Zhu Chenjian.C1~- TRACING METHOD IN ENVIRONMENTAL HYDROGEOLOGY[J].Periodical of Ocean University of China,1996(1).
Authors:Qiu Hanxue  Liu Guanqun  Shi Zhili  Li Tie  Zhu Chenjian
Abstract:The problems that we often meet in environmental geology such as groundwater pollution channel and extent, the influence range and degree of seawater intrusion, the character of groundwater dynamic field, etc, can be solved by using theC1- tracing method naturally or artificially. It is proved that C1- is a kind of natural and artifical groundwater movement tracing material by experiment for its special character that it is difficult to be adsorbed and does not take part in the chemical reaction in the vadose zone and moves easily in groundwater and vadose zone.
Keywords:Environmental hydrogeology  migration character of C1~-  C1~- tracing method  dynamic field analysis  pollution channel analysis  distinguishment of saline intrusion range
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