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张家口柴宣盆地浅层地下水水化学特征及水质评价
引用本文:陈迎辉,马苗苗,刘月东,闫佰忠,陈莹.张家口柴宣盆地浅层地下水水化学特征及水质评价[J].科学技术与工程,2024,24(7):3010-3019.
作者姓名:陈迎辉  马苗苗  刘月东  闫佰忠  陈莹
作者单位:河北省地质矿产勘查开发局第三地质大队;河北省水资源可持续利用与产业结构优化协同创新中心/河北地质大学水资源与环境学院
基金项目:河北省张承地区生态环境保护与修复技术创新中心项目(ZCZX201901);国家自然科学基金项目(42002251);河北省自然科学(Z20200033);河北省教育厅青年拔尖项目(BJK2022007)第一作者陈迎辉(1976-),男,汉族,河北张家口人,硕士,高级工程师。研究方向水文地质、环境地质。E-mail534424876@qq.com通讯作者马苗苗(2000-),女,汉族,河北省石家庄人,硕士,工程师。研究方向水文地质。E-mailmamiaomiao0620@163.com
摘    要:地下水作为张家口地区的主要供水水源,近年来受人类活动影响水质有恶化的趋势,影响了当地的用水安全,确定地下水化学特征与水质状况对水资源合理利用具有重要意义。基于2020年水质数据,选取Ca2+、Mg2+、K+、Na+、HCO-3、TH、pH、TDS、SO42-、Cl-、Al3+、NO-3、F-、Cr6+等水质因子,通过数理统计法、Piper三线图、Gibbs图和岩石风化端元图对张家口柴宣盆地地区浅层地下水水化学特征进行分析,并采用模糊综合评价和改进内梅罗指数法对水质进行评价。结果表明:研究区地下水是Ca2+和HCO-3为主的弱碱性淡水,微硬水、硬水和极硬水分别占39.51%、34.57%和25.93%;沿地下水流向,地下...

关 键 词:水化学特征  水质评价  模糊综合评价  改进内梅罗指数法  主成分分析  系统聚类分析  柴宣盆地
收稿时间:2023/4/19 0:00:00
修稿时间:2024/2/29 0:00:00

Hydrochemical Characteristics and Water Quality Evaluation of Shallow Groundwater in Chaixuan Basin, Zhangjiakou
Chen Yinghui,Ma Miaomiao,Liu Yuedong,Yan Baizhong,Chen Ying.Hydrochemical Characteristics and Water Quality Evaluation of Shallow Groundwater in Chaixuan Basin, Zhangjiakou[J].Science Technology and Engineering,2024,24(7):3010-3019.
Authors:Chen Yinghui  Ma Miaomiao  Liu Yuedong  Yan Baizhong  Chen Ying
Institution:No Geological Brigade of Hebei Geology And Mineral Exploration Bureau;Hebei Province Collaborative Innovation Center for Sustainable Utilization of Water Resources and Optimization of Industrial Structure/School of Water Resources Environment,Hebei GEO University
Abstract:As the main water supply source in Zhangjiakou area, the water quality of groundwater has deteriorated in recent years due to human activities, which has affected the local water safety. It is of great significance to find out the chemical characteristics and water quality of groundwater for rational utilization of water resources. Based on the water quality data of 2020, Ca2+, Mg2+, K+, Na+, HCO3-, TH, pH, TDS, SO42-, Cl-, Al3+, NO3-, F-, Cr6+ were selected as water quality factors. The hydro-chemical characteristics of shallow groundwater in the Chaixuan Basin of Zhangjiakou were analyzed by mathematical statistics, Piper diagram, Gibbs diagram and endmember diagram of rock weathering. The groundwater quality was evaluated by fuzzy comprehensive assessment and improved Nemerow index method. The results show that the groundwater in the study area is weakly alkaline freshwater dominated by Ca2+ and HCO3-, of which micro-hard water, hard water and hardest water account for 39.51%, 34.57% and 25.93%, respectively. The hydro-chemical types change from HCO3-Ca·Mg, HCO3-Na, SO4·Cl-Na to HCO3-Ca·Mg, HCO3-Na, SO4·Cl-Ca·Mg along the groundwater flow direction. The spatial distribution characteristics of hydro-chemical components are mainly affected by the weathering and dissolution of silicate and carbonate and human activities. The groundwater quality meets the standard of Class III on the whole, but the groundwater quality in some areas is poor. Along the flow direction of groundwater, the water quality gradually deteriorates, which is mainly affected by the primary geological environment and industrial and agricultural pollution.
Keywords:hydrochemical characteristics  water quality assessment  fuzzy complex index  improved Nemerow index method  principal component analysis  hierarchical cluster analysis  chaixuan Basin
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