德州南部高氟地下水水化学特征研究OA
Study on Hydrochemical Characteristics of High Fluoride Groundwater in Southern Dezhou City
高氟地下水是一种典型劣质水源,长期饮用可致人体患地方性高氟病.本次研究以禹城—平原地区为研究对象,对区内地下水进行氟含量、水化学类型和氟离子的影响因子等研究.结果表明,浅层地下水氟离子含量大部分不超过1.0mg/L,其水化学类型主要有HCO3-Na和Cl·SO4-Na型,深层地下水氟离子含量大部分均超过1.0mg/L,其水化学类型为HCO3·SO4-Na和HCO3·Cl-Na型.通过对pH和地下水水化学演化因素的研究,认为碱性环境一定程度能够促使氟离子聚集,但并不是唯一决定因子,高氟水的形成机制主要是水-岩相互作用和蒸发浓缩作用.
High fluorine groundwater is a typical poor quality water source.It can cause endemic high fluo-rine disease.In this study,taking Yucheng-Pingyuan area as the research object,the fluorine content,hydrochemical types and influence factors have been studied.It is showed that most of the fluorine content in shallow groundwater is not more than 1.0mg/L,and hydrochemical types are mainly HCO3-Na type and Cl·SO4-Na type.Most of the fluorine content in deep groundwater is more than 1.0mg/L,and hydrochemical types are HCO3·SO4-Na type and HCO3·Cl-Na type.Based on the study of pH and chemical evolution of groundwater,it is regarded that alkaline environment can promote fluorine ion ag-gregation to a certain extent.It is not the only decisive factor,and the formation mechanism of high fluo-rine water in this area are mainly water-rock interaction and evaporation concentration.
邵琦;刘晓震;董权德;左含月;刘伟;马立丹;韩玉冰;王炳凤
山东省地矿工程集团有限公司,山东济南 250200山东省地矿工程勘察院(八〇一水文地质工程地质大队),山东 济南 250014河北地质大学,河北 石家庄 050031山东省国土空间生态修复中心,山东济南 250014
地质学
高氟地下水影响因子水岩相互作用浓缩蒸发作用德州南部
High fluorine groundwaterinfluence factorswater-rock interactionconcentration and evap-oration effectsouth of Dezhou city
《山东国土资源》 2024 (003)
128-134 / 7
山东省自然资源厅2021年度省级地质勘查项目,山东省平原-禹城高氟区水文地质调查评价项目(鲁勘字[2021]47号)
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