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鲁西南平原高氟地下水水文地球化学特征
引用本文:冯超臣,黄文峰.鲁西南平原高氟地下水水文地球化学特征[J].山东国土资源,2005,21(5):39-42.
作者姓名:冯超臣  黄文峰
作者单位:1. 山东省鲁南地质工程勘察院,山东,兖州,272100
2. 菏泽市国土资源局,山东,菏泽,274000
摘    要:鲁西南地处黄河冲积平原,地势平坦,地下水运移迟缓,以垂直交替为主,氟离子含量较高,生活用水氟含量多大于1mg/L。局部地段地下水中氟含量可达7mg/L。高氟地下水在平面分布上具有点状和片状分布特点,在垂向上具有愈往深处氟含量愈高的特点。

关 键 词:高氟地下水  水文地球化学特征  鲁西南  地下水运移  氟含量  冲积平原  离子含量  生活用水  分布特点  平面分布
修稿时间:2004年6月7日

Hydro-geochemical Characteristics of Underground Water with High-fluorine in Southwest of Shandong Province
FENG Chao-chen and HUANG Wen-feng.Hydro-geochemical Characteristics of Underground Water with High-fluorine in Southwest of Shandong Province[J].Land and Resources in SHANDONG Province,2005,21(5):39-42.
Authors:FENG Chao-chen and HUANG Wen-feng
Abstract:Southwest area of Shandong province locates in Yellow river alluvial plain. Underground water flows very slowly and vertically with high fluorine content. Fluorine content included in living water is more than 1~ mg/L, while it can reach 7~ mg/L in some areas. Underground water has the distribution characteristics as spot and sheeting type, and fluorine content will become higher in deep part.
Keywords:Underground water  regional fluorsis  hydro-geochemistry  characteristics  southwest of Shandong province  
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