摘要
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1.0 mg/L,其水化学类型主要有HCO_(3)-Na和Cl·SO_(4)-Na型,深层地下水氟离子含量大部分均超过1.0 mg/L,其水化学类型为HCO_(3)·SO_(4)-Na和HCO_(3)·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 fluorine 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 HCO_(3)-Na type and Cl·SO_(4)-Na type.Most of the fluorine content in deep groundwater is more than 1.0mg/L,and hydrochemical types are HCO_(3)·SO_(4)-Na type and HCO_(3)·Cl-Na type.Based on the study of pH and chemical evolution of groundwater,it is regarded that alkaline environment can promote fluorine ion aggregation to a certain extent.It is not the only decisive factor,and the formation mechanism of high fluorine water in this area are mainly water rock interaction and evaporation concentration.
作者
邵琦
刘晓震
董权德
左含月
刘伟
马立丹
韩玉冰
王炳凤
SHAO Qi;LIU Xiaozhen;DONG Quande;ZUO Hanyue;LIU Wei;MA Lidan;HAN Yubing;WANG Bingfeng(Shandong Geo-engineering Exploration Limited Group,Shandong Ji'nan 250200,China;Shandong Geo-engineering Exploration Institute(No.801 Hydrogeological and Geo-engineering Brigade),Shandong Ji'nan 250014,China;Hebei University of Geosciences,Hebei Shijiazhuang 050031,China;Shandong Provincial Land Space Ecological Restoration Center,Shandong Ji'nan 250014,China)
出处
《山东国土资源》
2024年第3期128-134,共7页
Shandong Land and Resources
基金
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)。
关键词
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 groundwater
influence factors
water rock interaction
concentration and evaporation effect
south of Dezhou city
