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汾河流域地下水化学演化特征、控制因素及健康风险评价

李晓坚 苏贺 唐珧

人民黄河2025,Vol.47Issue(3):97-103,7.
人民黄河2025,Vol.47Issue(3):97-103,7.DOI:10.3969/j.issn.1000-1379.2025.03.015

汾河流域地下水化学演化特征、控制因素及健康风险评价

Hydrochemical Evolution Characteristics,Control Factors and Health Risk Assessment of Groundwater in the Fenhe River Basin

李晓坚 1苏贺 2唐珧1

作者信息

  • 1. 山西省水利发展中心,山西 太原 030002
  • 2. 太原理工大学,山西 太原 030024||河北省/中国地质调查局地下水污染机理与修复重点实验室,河北 石家庄 050061
  • 折叠

摘要

Abstract

The issue of groundwater pollution in the Fenhe River is becoming more and more serious and the water quality is deteriorating,resulting in the daily drinking water safety of residents in the Fenhe River Basin.In this paper,we selected groundwater in the Fenhe River Basin in the eastern part of the Loess Plateau as the research object,and comprehensively used mathematical statistics,graphical methods,correlation analysis,forward model,geographic detector and health risk assessment model to analyze the spatial-temporal evolution character-istics of groundwater chemistry,explore the formation mechanism of groundwater chemistry and quantify the contribution of different sources,identify the controlling factors of groundwater chemical evolution,and quantitatively evaluate the risks to human health through drinking wa-ter.The results show that the hydrochemical type of Fenhe River Basin evolves from HCO3-Ca to HCO3-Ca·Mg and SO4 HCO3-Ca·Mg;carbonate weathering and silicate weathering are the main sources of groundwater chemical composition.The main control factors of groundwa-ter chemical evolution are elevation and ecosystem,and ecosystem and land use.The non-carcinogenic risk factor of nitrate to children through drinking water is greater than that of adults.

关键词

地下水化学/时空演化/控制因素/健康风险/汾河

Key words

groundwater hydrochemistry/spatio-temporal variation/control factors/health risk/Fenhe River

分类

资源环境

引用本文复制引用

李晓坚,苏贺,唐珧..汾河流域地下水化学演化特征、控制因素及健康风险评价[J].人民黄河,2025,47(3):97-103,7.

基金项目

中国地质科学院水环所联合开放基金资助项目(SK202303) (SK202303)

山西省基础研究面上基金资助项目(202303021221020) (202303021221020)

人民黄河

OA北大核心

1000-1379

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