雄安新区浅层地下水化学成因及健康地质区划研究  

Study on hydrochemical origins and health geology regionalization of shallow groundwater in Xiong'an New Area

作　　者：夏雨波 王冰[4] 李海涛[5] 马震 郭旭 赵凯[5] 赵长荣 张曦[6] 王晓旭[7] XIA Yubo;WANG Bing;LI Haitao;MA Zhen;GUO Xu;ZHAO Kai;ZHAO Changrong;ZHANG Xi;WANG Xiaoxu(Tianjin Center(North China Center for Geoscience Innovation),China Geological Survey,Tianjin 300170,China;Tianjin Key Laboratory of Coast Geological Processes and Environmental Safety,Tianjin 300170,China;Xiong'an Urban Geological Research Center,China Geological Survey,Tianjin 300170,China;Tianjin Geothermal Exploration and Development-Designing Institute,Tianjin 300250,China;China Institute of Geo-Environment Monitoring,Beijing 100081,China;BGI Engineering Consultants Ltd.,Beijing 100038,China;Planning and Construction Bureau of Xiong'an New Area,Xiong'an 071799,Hebei,China)

机构地区：[1]中国地质调查局天津地质调查中心(华北地质科技创新中心),天津300170 [2]天津市海岸带地质过程与环境安全重点实验室,天津300170 [3]中国地质调查局雄安城市地质研究中心,天津300170 [4]天津地热勘查开发设计院,天津300250 [5]中国地质环境监测院,北京100081 [6]北京市勘察设计研究院有限公司,北京100038 [7]雄安新区规划建设局,河北雄安071799

出　　处：《中国地质》2025年第1期331-346,共16页Geology in China

基　　金：中国地质调查局项目(DD20189122、DD20189142、DD20190338、DD20221759)联合资助。

摘　　要：【研究目的】在水文地质实体内,生物生长和人群健康与周围环境、水土中的元素含量密切相关,研究地下水中与健康相关的宏微元素形成演化条件、建立健康地质区划,有利于推动健康中国战略的实施。【研究方法】本文选取雄安新区作为典型研究区,运用多元统计分析、Piper图和Chadha图等方法,分析浅层地下水水文地球化学特征及其物质成分来源,开展典型剖面上浅层地下水水质物源恢复,划定水化学类型分区,以环境和元素丰缺状况划分生物必须宏、微元素分异区,建立雄安新区健康地质分区划。【研究结果】研究区地下水各参数表现出高度变异性;水岩作用显示,钠长石的溶解为地下水贡献了Na+,萤石和石膏的溶解为地下水贡献了F^(−)和SO_(4)^(2−),消耗Ca^(2+)、Mg^(2+)和HCO_(3)^(−)析出了方解石、白云石,并发生了反向离子交换;研究区北部水化学类型以HCO_(3)–Ca、HCO_(3)–Ca·Mg型为主,过渡为中部HCO_(3)·SO_(4)–Na·Mg·Ca、HCO_(3)·Cl–Na·Ca·Mg、HCO_(3)·SO_(4)·Cl–Na·Mg型,递变为白洋淀及大清河下游的SO_(4)·HCO_(3)–Na·Mg型;雄安新区可分为北部冲洪积平原的元素缺乏健康地质分区、冲洪积平原与冲湖积平原交互地带的元素适中健康地质分区、冲湖积平原区的元素过剩健康地质分区3个分区,长时间饮用缺乏区和过剩区地下水会引起健康问题。【结论】需关注雄安新区由F^(−)、SO_(4)^(2−)、总硬度、I^(−)等浓度局部余缺引起或诱发的地方性疾病,需寻找替代水源或补充人体所需元素,为健康中国战略提供支撑。[Objective]In hydrogeological contexts,biological growth and human health are closely linked to the concentrations of elements present in the surrounding environment,including water and soil.Investigating the formation and evolutionary conditions of both macro and trace elements associated with health in groundwater,as well as establishing regional health geology,is beneficial for advancing the implementation of the Healthy China strategy.[Methods]Xiong'an New Area was chosen as the primary research site.The hydrogeochemical characteristics and sources of mineral composition in shallow groundwater were analyzed using multivariate statistical analysis,as well as the Piper and Chadha diagrams.This study restored the water quality by identifying the material element sources of shallow groundwater along a typical profile,delineated hydrochemical types,and classified the differentiation areas of macro and trace elements based on biological necessity,environmental factors,and element abundance or deficiency.Furthermore,it established a health geology regionalization for Xiong'an New Area.[Results]The parameters of groundwater exhibited significant variability.The water-rock interactions indicate that the dissolution of albite contributes sodium ions(Na+),while the dissolution of fluorite and gypsum contributes fluoride ions(F^(-))and sulfate ions(SO_(4)^(2−)),consuming calcium ions(Ca^(2+)),magnesium ions(Mg^(2+)),and bicarbonate ions(HCO_(3)^(−)),alongside the precipitation of calcite and dolomite,with reverse ion exchange also occurring.In the northern part of the study area,the predominant hydrochemical types were HCO_(3)–Ca and HCO_(3)–Ca·Mg.This composition transitioned to HCO_(3)·SO_(4)–Na·Mg·Ca,HCO_(3)·Cl–Na·Ca·Mg,and HCO_(3)·SO_(4)·Cl–Na·Mg in the middle section,ultimately evolving into SO_(4)·HCO_(3)–Na·Mg in Baiyangdian and downstream of the Daqing River.Xiong'an New Area can be categorized into three regions:A health geology regionalization characterized by a deficiency of element

关 键 词：水化学形成演化 地下水矿物分析 水文地球化学 雄安新区 健康地质 水文地质调查工程 

分 类 号：P641.12[天文地球—地质矿产勘探]