典型岩溶槽谷区地下水化学特征及地球化学敏感性分析  

Study of the chemical features and geochemical susceptibility of the groundwater system in a typical karst trough valley

作　　者：任坤[1,2,3] 师阳[1,2] 李晓春[4] 蓝家程[1,2] 徐尚全[1] 

机构地区：[1]西南大学地理科学学院/三峡库区生态环境教育部重点实验室,重庆400715 [2]国土资源部岩溶生态环境-重庆南川野外基地,重庆408435 [3]国土资源部广西壮族自治区岩溶动力学重点实验室,广西桂林541004 [4]西北大学资源与环境学院,陕西西安710127

出　　处：《中国岩溶》2014年第1期15-21,共7页Carsologica Sinica

基　　金：重庆市基础与前沿研究计划院士专项项目(cstc2013jcyjys20001);国家自然科学基金项目(41103068);2011年度重庆市国土房管局科技计划项目

摘　　要：利用2012年4月-2013年3月的水化学数据研究了重庆老龙洞地下河流域地下水系统地球化学敏感性。结果表明,研究区表层岩溶泉和地下河水化学阳离子分别以 Ca2＋、Mg2＋和 Ca2＋、Na＋为主,阴离子以 HCO-3、SO2-4为主；表层岩溶泉雨季 Mg2＋/Ca2＋摩尔比和地下河雨季 Na＋/Ca2＋摩尔比旱季大于雨季,表层岩溶泉和地下河雨季 HCO-3/SO2-4摩尔比分别为3.428-6.524、3.122-5.966,旱季 HCO-3/SO2-4摩尔比分别为5.693-8.664、3.428-6.524,表现出低SO2-4、高 HCO-3的特征,主要受农业活动影响的表层岩溶泉主量元素地球化学敏感性依次为 HCO-3＞ SO2-4＞Ca2＋＞NO-3＞ Mg2＋＞ Na＋＞ K＋＞Cl-,而受农业活动、工业活动、城镇建设活动等多种因子共同影响下的地下河主量元素地球化学敏感性有所变化,依次为 HCO-3＞Na＋＞ Ca2＋＞ K＋＞ Cl-＞ Mg2＋＞NO-3＞ SO2-4,随着人类影响的加剧,离子敏感指数将会有增加的趋势。The karst groundwater system is an important drinking water sources in karst regions.However, with urbanization development,groundwater in China has been widely polluted,especially karst groundwater in southwestern China.It is important to study the degree of response and mechanisms of groundwater fea-tures by external interference in order to guarantee drinking water safety.Using hydrochemical data for A-pril 2012 to March 2013,the geochemical susceptibility of groundwater in Laolongdong subterranean river and Zhaoj iayuanzi epi-karst spring in the river watershed of Nanshan,Chongqing was analyzed,and the prin-cipal cations were Ca2＋ and Mg2＋ in the epi-karst spring,and Ca2＋ and Na＋ in the subterranean river.The principal anions were HCO-3 and SO2-4 in both the subterranean river and the epi-karst spring.The values of Mg2＋/Ca2＋and Na＋/Ca2＋ were greater in the dry season than in rainy season.The value of HCO-3/SO2-4 was 5.693-8.664 and 3.428-6.524 in dry season,3.428-6.524 and 3.122-5.966 in rainy season.This indicates a high concentration of HCO-3 and low concentration of SO2-4 .Owing to agricultural activities,the rank order of geochemical susceptivity for major elements in the epi-karst spring is HCO-3 〉 SO2-4 〉 Ca2＋〉NO-3 〉 Mg2＋〉 Na＋〉 K＋〉 Cl-.When agricultural activities,industrial activities as well as urban con-struction activities were all taken into account,the rank order of geochemical susceptivity for maj or elements in the subterranean river became HCO-3 〉 Na＋〉 Ca2＋〉 K＋〉 Cl-〉 Mg2＋〉 NO-3 〉 SO2-4 .With an-thropic activities,each ion is becoming increasingly susceptive.Thus,more attention should be paid to karst groundwater pollution.

关 键 词：老龙洞地下河流域 地下水化学特征 地球化学敏感性 岩溶槽谷区 重庆 

分 类 号：P641.3[天文地球—地质矿产勘探] X131.2[天文地球—地质学]