银川平原地下水氟含量分布与成因及安全供水建议

    Distribution, Origin, and Safe Water Supply Implications of Fluoride in Groundwater of the Yinchuan Plain

    • 摘要: 医学研究表明,地下水中氟含量过高(>1.0mg/L)和过低(<0.5mg/L)都将对以地下水为饮用水源的群体的健康造成不同程度的危害,研究银川平原地下水氟含量分布与成因对安全供水意义重大。基于水文地质调查、地下水样品采集与地下水位观测,查明了氟含量分布特征;综合利用Piper图、Gibbs图和离子比值关系分析等方法,探讨了F−的来源及影响因素。结果表明,银川平原潜水氟含量0.11~5.18mg/L,承压水氟含量0.06~4.60mg/L,其中<0.5mg/L、0.5~1.0mg/L、>1.0mg/L样品数占比分别为49.02%、28.43%、22.55%和54.88%、27.07%、18.05%;水化学类型均以Cl•SO4-Na型为主。潜水、承压水氟含量分布均呈现黄河以东多为氟含量高值区,黄河以西则中间高两边低的特征。氟含量及其分布主要受岩石风化和蒸发浓缩作用及地下水径流条件控制,硅酸盐和蒸发岩矿物风化溶解是地下水中氟离子的主要来源,其次是碳酸盐矿物风化溶解,阳离子交换、引黄灌溉也是重要影响因素。本文以氟含量为指标将地下水划分为安全供水适宜区(0.5~1.0mg/L)、安全供水基本适宜区(<0.5mg/L)和安全供水不适宜区(>1.0mg/L)三个等级,并提出有针对性的安全供水措施,期待更多人关注和讨论,以服务于保障群众健康。

       

      Abstract: Medical studies indicate that both excessively high (>1.0 mg/L) and excessively low (<0.5 mg/L) fluoride (F⁻) content in groundwater can cause varying degrees of harm to the health of populations relying on it as a drinking water source. Therefore, studying the distribution and genesis of fluoride content in the groundwater of the Yinchuan Plain is of significant importance for ensuring safe water supply. Based on hydrogeological surveys, groundwater sample collection, and groundwater level monitoring, the distribution characteristics of fluoride content were identified. Comprehensive methods, including Piper diagrams, Gibbs diagrams, and ion ratio relationship analysis, were used to explore the sources and influencing factors of F⁻. The results show that the fluoride content in the shallow (unconfined) groundwater of the Yinchuan Plain ranges from 0.11 to 5.18 mg/L, while in the confined groundwater it ranges from 0.06 to 4.60 mg/L. The proportion of samples with F⁻ concentrations <0.5 mg/L, 0.5–1.0 mg/L, and >1.0 mg/L is 49.02%, 28.43%, and 22.55% for shallow groundwater, and 54.88%, 27.07%, and 18.05% for confined groundwater, respectively. The predominant hydrochemical type for both is Cl·SO₄-Na. The fluoride distribution in both shallow and confined groundwater shows a pattern where areas east of the Yellow River are mostly high-value zones, while areas west of the river exhibit higher values in the central part and lower values on either side. Fluoride content and its distribution are primarily controlled by rock weathering, evaporation concentration, and groundwater flow conditions. The weathering and dissolution of silicate and evaporite minerals are the main sources of fluoride ions in groundwater, followed by carbonate mineral weathering and dissolution. Cation exchange and Yellow River irrigation are also significant influencing factors. Based on fluoride content as an indicator, the groundwater is classified into three safety levels for water supply: Suitable Area (0.5–1.0 mg/L), Relatively Suitable Area (<0.5 mg/L), and Unsuitable Area (>1.0 mg/L). Targeted safe water supply measures are proposed. It is hoped this study will draw more attention and discussion to serve the goal of safeguarding public health.

       

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