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鲁西南黄河下游地下水氟富集规律及其影响因素

孟甲 郑慧铭 宋帅良 张茜 张丰

地质通报2024,Vol.43Issue(9):1663-1672,10.
地质通报2024,Vol.43Issue(9):1663-1672,10.DOI:10.12097/gbc.2023.07.006

鲁西南黄河下游地下水氟富集规律及其影响因素

Fluorine enrichment pattern of groundwater in the lower reaches of the Yellow River in southwestern Shandong Province and influencing factors

孟甲 1郑慧铭 2宋帅良 2张茜 2张丰1

作者信息

  • 1. 山东省鲁南地质工程勘察院(山东省地质矿产勘查开发局第二地质大队),山东济宁 272100||山东省地矿局岩溶地质重点实验室,山东济宁 272100
  • 2. 山东省鲁南地质工程勘察院(山东省地质矿产勘查开发局第二地质大队),山东济宁 272100
  • 折叠

摘要

Abstract

The southwestern plain of Shandong Province is located in the lower reaches of the Yellow River,and there are few studies on the chemical genesis of groundwater in this region and the mechanism of its influence on fluorine enrichment in groundwater at this stage.In this study,36 shallow groundwater samples,16 deep groundwater samples and 2 Yellow River water samples were collected for comprehensive analysis and testing.By means of statistical,correlation analysis and water chemistry simulation,the chlor-alkali index(CAI),Durov diagram,Gibbs diagram,Ca2+/Na+-Mg2+/Na+diagram,log10(Ca2+)activity-log10(F-)activity diagram were constructed,and then the causes of groundwater chemistry and its fluoride enrichment mechanism in the study area were analyzed.The results showed that the chemical types of both shallow and deep groundwater in the study area were mainly HCO3-Na,indicating the overall alkaline,the fluorine content of groundwater was 1.59 mg/L and 2.35 mg/L,respectively,and the level of fluorine content in deep water varied less than that in shallow water.The fluorine content in shallow groundwater in the area was significantly negatively correlated with Ca2+content and positively correlated with pH value.The fluorine content in deep groundwater was significantly and positively correlated with Na+and TDS values.The chemical composition of groundwater in the study area is mainly controlled by water-rock action and cation exchange,and the fluorine content of groundwater mainly comes from the dissolution of fluorite(CaF2),and is controlled by Ca2+content.This study revealed the fluorine enrichment laws and influencing factors in the main groundwater aquifers in the lower reaches of the Yellow River.

关键词

黄河下游/鲁西南/冲积平原/高氟地下水/水化学/阳离子交换

Key words

lower Yellow River/southwest of Shandong/alluvial plains/high fluorine groundwater/hydrochemistry/cation exchange

分类

天文与地球科学

引用本文复制引用

孟甲,郑慧铭,宋帅良,张茜,张丰..鲁西南黄河下游地下水氟富集规律及其影响因素[J].地质通报,2024,43(9):1663-1672,10.

基金项目

山东省自然资源厅省级地质勘查项目《菏泽黄河滩区生态地质调查》(编号:鲁勘字[2020]51号) (编号:鲁勘字[2020]51号)

地质通报

OA北大核心CSTPCD

1671-2552

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