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珠江三角洲浅层地下水pH值的分布及成因浅析

张玉玺 孙继朝 陈玺 黄冠星 荆继红 刘景涛 向小平 王金翠 支兵发

水文地质工程地质2011,Vol.38Issue(1):16-21,6.
水文地质工程地质2011,Vol.38Issue(1):16-21,6.

珠江三角洲浅层地下水pH值的分布及成因浅析

Characteristics and preliminary analyses of the formation of pH in shallow groundwater in the Pearl River delta

张玉玺 1孙继朝 1陈玺 1黄冠星 1荆继红 1刘景涛 1向小平 1王金翠 1支兵发2

作者信息

  • 1. 中国地质科学院水文地质环境地质研究所,石家庄,050061
  • 2. 广东省地质调查院,广州,510080
  • 折叠

摘要

Abstract

More than 2,000 groundwater samples were detected in situ for pH in the Pearl River Delta.The results show that water acidification is the most prominent problem in the groundwater environment.Acidic groundwater accounts for 76.3% of the total area.Distribution of pH in the shallow groundwater is of obvious regional characteristics.In the hilly areas, pH in groundwater ranges mostly from 5.6 to 6.4, while pH varies mainly between 6.4 and 7.2 in the plain regions.Due to the influence of acid rain, pH of groundwater is slightly lower in wet season than in dry season.It is considered that acid rain and medium buffer of unsaturated zone play an important role in the lower pH value in groundwater in the hilly areas.In the plain areas, the acid rainfall infiltration coefficient becomes lower, while rivers and seawater tide are the dominant factors causing higher pH values of the groundwater.

关键词

珠江三角洲/浅层地下水/pH 值

分类

天文与地球科学

引用本文复制引用

张玉玺,孙继朝,陈玺,黄冠星,荆继红,刘景涛,向小平,王金翠,支兵发..珠江三角洲浅层地下水pH值的分布及成因浅析[J].水文地质工程地质,2011,38(1):16-21,6.

基金项目

珠江三角洲地下水污染调查评价专题研究(1212010534807) (1212010534807)

水文地质工程地质

OA北大核心CSCDCSTPCD

1000-3665

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