北京大兴区第四系高氟地下水分布规律研究

现代地质 ›› 2012, Vol. 26 ›› Issue (2): 407-414.

北京大兴区第四系高氟地下水分布规律研究

李世君^1,2, 王新娟³, 周俊², 汤新梅^3,4, 王兆萄⁵

1 中国地质大学水资源与环境学院，北京100083；2 北京市地质工程勘察院，北京100048；3 北京市水文地质工程地质大队，北京100195；4 吉林大学环境与资源学院，吉林长春130012；5 通辽市防汛抗旱物资供应管理站，内蒙古通辽028000

收稿日期:2011-09-27 修回日期:2011-12-30 出版日期:2012-04-20 发布日期:2018-09-19
作者简介:李世君，男，高级工程师，博士研究生，1972年出生，水文地质学专业，主要从事地下水资源和水环境评价工作。Email：lisj5@163.com。
基金资助:
北京市地质工程勘察院水资源地质调查项目“大兴区第四系地下水分布地下水资源调查研究”。

Distribution Law of High Fluoride Groundwater in Quaternary in Daxing District of Beijing

LI Shi-Jun^-1,2, WANG Xin-Juan^-3, ZHOU Dun^-2, SHANG Xin-Mei^-3,4, WANG Zhao-Tao^-5

1 School of Water Resources and Environment, China University of Geosciences, Beijing100083,China；2 Beijing Institute of Geological Engineering, Beijing100048,China；3 Hydrogeological and Engineering Geological Team of Beijing, Beijing100195,China；4 College of Environment and Resources, Jilin University, Changchun, Jilin130012, China;5 Tongliao Management Station of Material Supply for Flood Control and Drought Resistance, Tongliao, Inner Mongolia028000,China)

Received:2011-09-27 Revised:2011-12-30 Online:2012-04-20 Published:2018-09-19

摘要/Abstract

摘要：

北京市大兴区供水以地下水为主，研究该区高氟地下水的分布规律及其成因，对指导区域地下水的开发利用和保障居民饮水安全是必要的。在野外调查和以往研究成果的基础上，测试了北京大兴区地下水氟离子浓度。结果表明，高氟水分布区地层岩性以粘性土为主；浅层高氟水主要分布在大兴区的南部及东南部，超标区面积为258.57 km²；深层高氟水主要分布在中部，超标区面积为20.91 km²。建议对浅层高氟地下水加大止水深度，统一并严格设计饮用水井结构；对深层氟超标水，避免饮用或采取降氟措施后再饮用。

关键词: 高氟水, 分布规律, 第四系, 北京大兴区

Abstract:

Water supply in Daxing district of Beijing mainly comes from groundwater, and it is necessary to discuss the distribution law and genesis of high fluorine groundwater for guiding groundwater development and ensuring drinking water safety. Based on field survey and previous research, concentrations of fluoride ion of groundwater from Daxing district of Beijing are measured. The results show that high fluorine water is distributed mainly in cohesive soil, that high fluorine water of shallow layer with 258.57 km² exceeding fluorine national standard is distributed mainly in south and eastsouth of Daxing district, and that high fluorine water is distributed mainly in central section with 20.91 km² exceeding fluorine national standard. Two suggestions are given in this paper as the following: (1) the stopdepth of shallow highfluoride water should be increased, and the structure of drinking water wells should be strictly integrated and designed; (2) the deep highfluoride water should avoid being drunk or should be drunk after decreasing fluoride content.

Key words: high fluoride groundwater, distribution law, Quaternary；Daxing district of Beijing

李世君, 王新娟, 周俊, 汤新梅, 王兆萄. 北京大兴区第四系高氟地下水分布规律研究[J]. 现代地质, 2012, 26(2): 407-414.

LI Shi-Jun, WANG Xin-Juan, ZHOU Dun, SHANG Xin-Mei, WANG Zhao-Tao. Distribution Law of High Fluoride Groundwater in Quaternary in Daxing District of Beijing[J]. Geoscience, 2012, 26(2): 407-414.

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