郯庐断裂带南段高氟地热水成因机制及健康风险评价

    Genetic mechanism of fluoride-enriched geothermal groundwater in the southern segment of Tanlu fault and human health risk assessment

    • 摘要: 郯庐断裂带南段的地热水中氟离子含量较高,为助力郯庐断裂带南段地热资源实现科学开发与可持续利用,亟需明确该区域高氟地热水的循环演化机制与成藏模式,并评估其健康风险。基于在断裂带南段采集的11组水样,综合运用水化学分析、氢氧同位素测试、水文地球化学图解及离子比例关系法,系统识别了地热水与地下水的空间分布规律及水化学特征,进而深入探究深大断裂沿线高氟地热水的循环演化过程与成藏条件。结果表明: 研究区地下水为HCO3-Ca型,呈酸性; 地热水则以SO4-Na型为主,呈碱性,高氟水主要赋存于地热水中,F-浓度超出国家饮用水标准2~12倍,而地下水中F含量未超标; 地热水主要接受大气降水补给,补给高程为1 116~1 453 m,循环深度为1 259~1 534 m,经石英温标估算热储温度为106.5~119.2 ℃; 高氟地热水化学特征受多种水文地球化学作用叠加影响,富氟矿物风化与溶解是氟含量偏高的主导因素,碱性地热水环境及阳离子交换作用间接促进了F-的富集。健康风险评价显示,高氟地热水对儿童的潜在危害显著高于成年女性和成年男性。上述结果明确了郯庐断裂带南段高氟地热水的循环演化机制与成藏模式,揭示了富氟成因及人群健康风险差异,为区域地热资源的合理开发与可持续利用提供了科学依据,同时强调了高氟地热水对不同年龄段人群的差异化影响,对保障当地居民尤其是儿童的饮用水安全具有重要现实意义。

       

      Abstract: The geothermal water has excessive fluoride concentrations in the southern segment of Tanlu Fault. In order to support the scientific development and sustainable utilization of geothermal resources in the southern segment of Tanlu Fault, the authors explored the evolution mechanisms, and formation patterns of high-fluoride geothermal water, and evaluated the health risk. Eleven water samples were collected in the southern segment of TanLu Fault, and geothermal water distribution and characteristics were identified via hydrochemistry, hydrogen/oxygen isotope testing, hydrogeochemical diagrams and ion ratio analysis. Besides, the cycle process and reservoir forming condition of the fluoride-enriched geothermal water along Tanlu Fault were explored. The results show that the local groundwater is HCO3-Ca type (acidic), while geothermal water is mostly SO4-Na type (alkaline). The fluoride-enriched water occurs mainly in geothermal reservoirs, with the fluoride levels exceeding national standards by 2~12 times. While the groundwater fluoride levels are within limits. The geothermal water is mainly recharged by atmospheric precipitation at 1 116~1 453 m elevation, circulating at 1 259~1 534 m depth, and reservoir temperature of 106.5~119.2 ℃ (via quartz geothermometry). The fluoride-enriched geothermal water chemistry is shaped by multiple hydrogeochemical processes. Fluoride-enriched mineral weathering/dissolution is the main cause of high fluoride, while alkaline conditions and cation exchange also contribute to fluoride accumulation. Health risk assessment shows that high-fluoride geothermal water poses a greater potential risk to children than to adult women/men. The evolution mechanisms and formation patterns of high-fluoride geothermal water in the southern segment of Tanlu Fault were defined, and the causes of high fluoride and health risk differences were revealed, providing scientific basis for local geothermal resource management. The differential health impacts of high-fluoride geothermal water on different populations were emphasized and it is highly significant for ensuring local residents' water safety, particularly for children.

       

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