文章摘要
孙一博, 刘朋飞, 王文科.关中盆地浅层地下水水化学空间分布规律的研究Journal of Water Resources and Water Engineering[J].,2015,26(3):20-23
关中盆地浅层地下水水化学空间分布规律的研究
Study on spatial distribution law of hydrochemistry in shallow groundwater of Guanzhong basin
  
DOI:10.11705/j.issn.1672-643X.2015.03.005
中文关键词: 浅层地下水  水化学特征  空间分布规律  关中盆地
英文关键词: shallow groundwater  hydro-chemical feature  spatial distribution law  Guanzhong Basin
基金项目:中国地质调查局地质大调查计划项目(1212010634700)
Author NameAffiliation
SUN Yibo1, LIU Pengfei2, WANG Wenke3 (1.重庆市地勘局南江水文地质工程地质队 重庆 401121 2.中铁二院重庆勘察设计研究院有限责任公司重庆 400023
3.长安大学 环境科学与工程学院
陕西 西安 710054) 
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中文摘要:
      从水化学角度出发,利用关中盆地浅层地下水164组水化学分析数据,分析了关中盆地浅层地下水的水化学特征及水循环规律。结果表明:关中盆地浅层地下水水化学类型呈现明显的水平分布特征,渭河以南及渭北泾河以西浅层地下水主要以HCO-3型水为主,水化学类型简单,矿化度多小于1 g/L;渭北泾河以东浅层地下水有Cl-、SO42-型水,水化学类型复杂,矿化度较高;TDS与Na+、Cl-、SO42-呈正相关性;浅层地下水具有河谷型和盆地型的双重特征。
英文摘要:
      From the perspective of water chemistry,the paper used hydrochemistry data of 164 groups in shallow groundwater of Guanzhong Basin to analyze water chemical characteristics and law of water cycle.The result showed that water chemical types present obvious horizontal distribution characteristics.At the south of Weihe river and the west of Jinghe river,the shallow groundwater is main HCO3 type water and its hydrochemical type is simple,and salinity is much less than 1g/L; at the east of Jinghe river,there are Cl-、SO42- type water exposed in shallow groundwater, the hydrochemical type is complex and salinity is higher; TDS have positive correlation with Na+,Cl- and SO42-;shallow groundwater has the double features of valley and basin type.
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