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新密市双洎河流域超化段地下水化学演变特征

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[目的]地下水是新密市超化镇的重要用水来源.研究新密市双洎河流域超化段岩溶地下水化学类型的历史演变特征,可为地下水的安全管理使用提供科学依据.[方法]通过收集20世纪60年代、80年代和2021年的地下水化学资料,进行地下水化学组分的历史演变特征对比分析.[结果]研究区岩溶地下水化学类型主要为HCO3-Ca型和HCO3-Ca·Mg型水.多年来,研究区大部分岩溶地下水的水化学类型没有改变.相较于20世纪,2021年研究区整体TDS水平有所增高,局部岩溶地下水中的Na+和SO42-含量上升,地下水化学类型种类增多.[结论]岩溶水化学组分的变化与地表水的下渗补给等自然条件和煤矿开采、采空区的形成等人类影响关系密切.污染通道的封堵和定期的水质监测是保护岩溶地下水的重要措施.
Characteristics of Groundwater Chemical Evolution in the ChaoHua Section of Shuangji River Basin in Xinmi City
[Purposes]Groundwater is an important source of water for Chaohua Town in Xinmi City,and its hydrochemical composition directly affects the water safety and quality of life of residents.[Methods]In order to search the historical evolution characteristics of karst groundwater chemical types in the Chaohua section of the Shuangji River Basin in Xinmi City,this article collected groundwater chemical data from the 1960s,1980s,and 2021,and conducted a comparative analysis of the historical evolution characteristics of groundwater chemical components.[Findings]The results indicate that:The chemical types of karst groundwater in the study area are mainly HCO3-Ca type and HCO3-Ca·Mg type water.And the types have not changed over the years.Compared to the previous century,the overall TDS level in the study area increased in 2021,with an increase in the content of Na+ and SO42-in local karst ground-water and an increase in the types of groundwater chemical types.[Conclusions]The changes in the chemical composition of karst water are closely related to natural conditions such as surface water infil-tration,as well as human impacts such as coal mining and goaf formation.Blocking pollution channels and regular water quality monitoring are important measures to protect karst groundwater.

groundwaterchemical types of groundwaterChaohua section of Shuangji River Basinchar-acteristics of evolution

何欣琳、孙学静、苏建仓、占亮

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河南省地质研究院,河南 郑州 450016

河南省地下水污染防治与修复重点实验室,河南郑州 450001

地下水 地下水化学类型 双洎河流域超化段 演变特征

中央水污染防治资金项目

2020410183S1-40001

2024

河南科技
河南省科学技术信息研究院

河南科技

影响因子:0.615
ISSN:1003-5168
年,卷(期):2024.51(5)
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