荥巩矿区岩溶地下水系统的水文地球化学特征及其指示意义  

Characteristics and indication of hydrogeochemisty for the karst groundwater system in the Xinggong coal field

作　　者：张群利[1] 郭会荣[1] 吴孔军[1,2] 韩国童 

机构地区：[1]中国地质大学环境学院,武汉430074 [2]河南省地质矿产勘查开发局测绘队,郑州450006

出　　处：《水文地质工程地质》2011年第2期1-7,共7页Hydrogeology & Engineering Geology

基　　金：国家自然科学基金项目(40772155);863计划(2007AA06Z337)

摘　　要：本文在分析荥巩矿区水文地质条件的基础上,重点对岩溶地下水系统的水化学特征进行分析。结果表明:岩溶水水化学类型自补给区到排泄区,从单一的HCO3型向复杂的HCO3.SO4型和SO4.HCO3型转变,TDS和Sr2+/Ca2+值均增加。地下水氢氧稳定同位素分析结果表明,本区岩溶地下水主要接受大气降水的入渗补给。根据同位素计算的补给高程推断岩溶水补给范围和划分的流动系统与地面调查结果及水化学研究成果一致:矿区处于区域流动系统排泄带,中寒武统张夏组—中奥陶统灰岩在矿区南部出露的范围接受降水补给,以侧向径流的方式进入矿区充水含水层。Based on a regional hydrogeological survey,the hydrogeochemical characteristics of a karst groundwater system in the Xinggong coal field were analyzed in this paper.The results show that from recharge zones to discharge zones,the hydrochemical type of groundwater changes from HCO3-Ca（Mg） to HCO3.SO4-Ca（Mg） or SO4.HCO3-Ca（Mg） type,TDS and the ratio of Sr2 ＋ to Ca2 ＋ in groundwater increase.Isotopic characteristics indicate that groundwater is mainly recharged from modern precipitation.The recharge elevation calculated with isotopes and the flowing system divided by hydrogeological surveys are coincide with the conclusions drawn from water chemistry analysis for the karst groundwater.Namely,the coal field is in the discharge zone of the regional flow systems;the groundwater in the limestone formations（∈2z-O2m） exposed in the south of the coal field is recharged by the precipitation,then flows to northern coal field where the O2m aquifer is underlain by the coal formation.In the coal field the groundwater moves through a long distance and the velocity is slower than that in the recharge zone.As a result,the water quality is more complex than that in the recharge zone.

关 键 词：水化学特征 氢氧稳定同位素 岩溶水流动系统 荥巩矿区 

分 类 号：P641.3[天文地球—地质矿产勘探]