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运用自组织映射识别中低温富氟地热水的遗传机制,并评估中国东南部武功山地区的健康风险。

Identifying the genetic mechanism of medium-low temperature fluoride-enriched geothermal groundwater by the self-organizing map and evaluating health risk in the Wugongshan area, southeast China.

机构信息

Chinese Academy of Geological Sciences, Beijing, 100037, China.

School of Water Resources and Environment, China University of Geosciences, Beijing, 100083, China.

出版信息

Environ Geochem Health. 2024 Jul 3;46(8):274. doi: 10.1007/s10653-024-02058-4.

Abstract

Fluoride-enriched groundwater is a serious threat for groundwater supply around the world. The medium-low temperature fluoride-enriched geothermal groundwater resource is widely distributed in the circum-Wugongshan area. And the fluoride concentration of all geothermal samples exceeds the WHO permissible limit of 1.5 mg/L. The Self-Organizing Map method, hydrochemical and isotopic analysis are used to decipher the driving factors and genetic mechanism of fluoride-enriched geothermal groundwater. A total of 19 samples collected from the circum-Wugongshan geothermal belt are divided into four clusters by the self-organizing map. Cluster I, Cluster II, Cluster III, and Cluster IV represent the geothermal groundwater with the different degree of fluoride concentration pollution, the different hydrochemical type, and the physicochemical characteristic. The high F concentration geothermal groundwater is characterized by HCO-Na with alkalinity environment. The δD and δO values indicate that the geothermal groundwater origins from the atmospheric precipitation with the recharge elevation of 1000-2100 m. The dissolution of fluoride-bearing minerals is the main source of fluoride ions in geothermal water. Moreover, groundwater fluoride enrichment is also facilitated by water-rock interaction, cation exchange and alkaline environment. Additionally, the health risk assessment result reveals that the fluorine-enriched geothermal groundwater in the western part of Wugongshan area poses a more serious threat to human health than that of eastern part. The fluoride health risks of geothermal groundwater for different group show differentiation, 100% for children, 94.74% for adult females, and 68.42% for adult males, respectively. Compared with adult females and adult males, children faced the greatest health risks. The results of this study provide scientific evaluation for the utilization of geothermal groundwater and the protection of human health around the Wugongshan area.

摘要

富氟地下水是世界各地地下水供应的严重威胁。中低温富氟地热水资源广泛分布于武功山周边地区,所有地热水样的氟浓度均超过世界卫生组织规定的 1.5mg/L 限值。本研究采用自组织映射方法、水化学和同位素分析,解析富氟地热水的成因机制。共采集武功山周边地热带 19 个水样,利用自组织映射将其分为 4 类。聚类 I、聚类 II、聚类 III 和聚类 IV 分别代表氟浓度污染程度不同、水化学类型不同和具有不同物理化学特征的地热水。高 F 浓度地热水的特征是具有碱性环境的 HCO-Na 型。δD 和 δO 值表明,地热水来源于大气降水,补给高程为 1000-2100m。含氟矿物的溶解是地热水中氟离子的主要来源。此外,水岩相互作用、阳离子交换和碱性环境也促进了地下水氟的富集。另外,健康风险评估结果表明,武功山地区西部富氟地热水对人体健康的威胁比东部更为严重。不同群体地热水的氟健康风险存在差异,儿童为 100%,成年女性为 94.74%,成年男性为 68.42%。与成年女性和成年男性相比,儿童面临的健康风险最大。本研究结果为武功山地区地热水的利用和人类健康保护提供了科学评价。

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