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河北省张北县新生代玄武岩偏硅酸矿泉水化学特征及成因

何锦 马雪梅 邓启军 李伟 马学军 郑一迪 刘昭

中国地质2023,Vol.50Issue(6):1887-1902,16.
中国地质2023,Vol.50Issue(6):1887-1902,16.DOI:10.12029/gc20201027001

河北省张北县新生代玄武岩偏硅酸矿泉水化学特征及成因

Hydrochemical characteristics and formation mechanism of metasilicate mineral water in a Cenozoic basaltic aquifer in Zhangbei county,Hebei Province

何锦 1马雪梅 2邓启军 2李伟 2马学军 2郑一迪 2刘昭3

作者信息

  • 1. 中国地质调查局水文地质环境地质调查中心,河北保定 071051||吉林大学新能源与环境学院,吉林长春 130026
  • 2. 中国地质调查局水文地质环境地质调查中心,河北保定 071051
  • 3. 河北地质大学水资源与环境学院,河北石家庄 050031
  • 折叠

摘要

Abstract

This paper is the result of hydrogeological survey engineering. [Objective]Metasilicate mineral groundwater is widely distributed in cenozoic basaltic stratum of Bashang area.It is of great practical significance to study the formation mechanism and water-rock interaction for rational utilization of water resources and development of mineral water industry in this area.[Methods]The formation mechanism of metasilicate mineral groundwater in Cenozoic basalt in the research area was analyzed by collecting environmental hydrochemical samples such as groundwater and rainwater systematically and using mathematical statistics,ion ratio analysis,isotope analysis and other methods.[Results]The metasilicate mineral water is mainly distributed in the groundwater recharge area of the front edge in the Bashang area on southern part of the county;And the mineral groundwater of study area is characterized by low mineralization while the main hydrochemical types of groundwater are HCO3-Ca·Mg and HCO3-Na·Ca;Also,metasilicic acid in groundwater originates from the hydrolysis of sodaclase,plagioclase,olivine and other silicate mineral in basalt,and is affected by rock mineral leaching as well as hydrochemical parameters cation exchange.According to the analytical results of hydrogen-oxygen isotope,it is concluded that the main source of groundwater recharge is local precipitation in summer,and the actual age of groundwater is between 15 a and 60 a.[Conclusions]The formation of metasilicate mineral water in Bashang area of Hebei Province is related to the local special basalt geological structure and specific hydrogeochemical process.

关键词

偏硅酸矿泉水/玄武岩/水文地球化学/稳定同位素/水文地质调查工程/张北县/河北省

Key words

metasilicate mineral water/basalts/hydrochemistry/stable isotopes/hydrogeological survey engineering/Zhangbei county/Hebei Province

分类

天文与地球科学

引用本文复制引用

何锦,马雪梅,邓启军,李伟,马学军,郑一迪,刘昭..河北省张北县新生代玄武岩偏硅酸矿泉水化学特征及成因[J].中国地质,2023,50(6):1887-1902,16.

基金项目

中国地质调查局项目(DD20160328)资助. Supported by the project of China Geological Survey"Comprehensive Geological Survey of the Northern Section of Taihang Mountain"(No.DD20160328). (DD20160328)

中国地质

OA北大核心CSCDCSTPCD

1000-3657

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