地热水中的氟化物:赋存、来源、迁移及环境影响

IF 3.3 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Journal of Geochemical Exploration Pub Date : 2025-03-01 Epub Date: 2024-11-26 DOI:10.1016/j.gexplo.2024.107640
Xuelian Huang , Shuai Wang , Sijia Wang , Zhicai Xiao , Min Zhang , Hongyan Zhang , Shihua Qi
{"title":"地热水中的氟化物:赋存、来源、迁移及环境影响","authors":"Xuelian Huang ,&nbsp;Shuai Wang ,&nbsp;Sijia Wang ,&nbsp;Zhicai Xiao ,&nbsp;Min Zhang ,&nbsp;Hongyan Zhang ,&nbsp;Shihua Qi","doi":"10.1016/j.gexplo.2024.107640","DOIUrl":null,"url":null,"abstract":"<div><div>Geothermal water, a vital renewable energy source extensively harnessed for heating and power generation, is marred by a prevalent issue – high fluoride content. The environmental impact of geothermal fluoride has been recognized globally. The natural discharge of geothermal water, coupled with its widespread exploitation, instigates the translocation of geothermal fluoride toward shallow and surface water ecosystems, culminating in escalating fluoride concentrations, thereby posing potential threats to both ecosystems and human health. Nevertheless, despite the pivotal significance of fluoride in geothermal water, a comprehensive understanding of its origins, migratory dynamics, ecological consequences, and ameliorative methodologies remains to be studied. This review provides a comprehensive examination of fluoride's global occurrence and distribution in geothermal waters, emphasizing the contrast between volcanic and non-volcanic geothermal systems. It analyzes the various sources of fluoride in these waters and elucidates the mechanisms driving its mobilization. In volcanic geothermal systems, fluoride primarily derives from magmatic volatiles, while in non-volcanic systems, it mainly results from the dissolution of minerals. Temperature is a key factor influencing fluoride concentration in geothermal waters, with alkaline conditions and low calcium levels contributing to higher fluoride enrichment. The review details how fluoride concentrations change as geothermal fluids migrate from deeper to shallower layers. Based on the enrichment characteristics of fluorides, this paper explores the potential applications of geothermal fluorides. It also examines the environmental impacts of geothermal fluoride, presents various treatment methods, and provides a summary of current research both domestically and internationally, while proposing directions for future studies. This study is instrumental in formulating judicious fluoride management policies and establishing sustainable strategies for the development of geothermal resources.</div></div>","PeriodicalId":16336,"journal":{"name":"Journal of Geochemical Exploration","volume":"270 ","pages":"Article 107640"},"PeriodicalIF":3.3000,"publicationDate":"2025-03-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Fluoride in geothermal water: Occurrence, origin, migration and environmental impact\",\"authors\":\"Xuelian Huang ,&nbsp;Shuai Wang ,&nbsp;Sijia Wang ,&nbsp;Zhicai Xiao ,&nbsp;Min Zhang ,&nbsp;Hongyan Zhang ,&nbsp;Shihua Qi\",\"doi\":\"10.1016/j.gexplo.2024.107640\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Geothermal water, a vital renewable energy source extensively harnessed for heating and power generation, is marred by a prevalent issue – high fluoride content. The environmental impact of geothermal fluoride has been recognized globally. The natural discharge of geothermal water, coupled with its widespread exploitation, instigates the translocation of geothermal fluoride toward shallow and surface water ecosystems, culminating in escalating fluoride concentrations, thereby posing potential threats to both ecosystems and human health. Nevertheless, despite the pivotal significance of fluoride in geothermal water, a comprehensive understanding of its origins, migratory dynamics, ecological consequences, and ameliorative methodologies remains to be studied. This review provides a comprehensive examination of fluoride's global occurrence and distribution in geothermal waters, emphasizing the contrast between volcanic and non-volcanic geothermal systems. It analyzes the various sources of fluoride in these waters and elucidates the mechanisms driving its mobilization. In volcanic geothermal systems, fluoride primarily derives from magmatic volatiles, while in non-volcanic systems, it mainly results from the dissolution of minerals. Temperature is a key factor influencing fluoride concentration in geothermal waters, with alkaline conditions and low calcium levels contributing to higher fluoride enrichment. The review details how fluoride concentrations change as geothermal fluids migrate from deeper to shallower layers. Based on the enrichment characteristics of fluorides, this paper explores the potential applications of geothermal fluorides. It also examines the environmental impacts of geothermal fluoride, presents various treatment methods, and provides a summary of current research both domestically and internationally, while proposing directions for future studies. This study is instrumental in formulating judicious fluoride management policies and establishing sustainable strategies for the development of geothermal resources.</div></div>\",\"PeriodicalId\":16336,\"journal\":{\"name\":\"Journal of Geochemical Exploration\",\"volume\":\"270 \",\"pages\":\"Article 107640\"},\"PeriodicalIF\":3.3000,\"publicationDate\":\"2025-03-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Geochemical Exploration\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0375674224002565\",\"RegionNum\":2,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"2024/11/26 0:00:00\",\"PubModel\":\"Epub\",\"JCR\":\"Q1\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Geochemical Exploration","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0375674224002565","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"2024/11/26 0:00:00","PubModel":"Epub","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0

摘要

地热水是一种重要的可再生能源,广泛用于供暖和发电,但它存在一个普遍问题,即氟化物含量高。地热氟化物对环境的影响已在全球得到承认。地热水的自然排放,加上地热水的广泛开采,促使地热氟化物向浅水和地表水生态系统转移,最终导致氟化物浓度不断上升,从而对生态系统和人类健康构成潜在威胁。然而,尽管地热水中的氟化物具有关键意义,但对其起源、迁移动态、生态后果和改进方法的全面了解仍有待研究。本文综述了全球地热水中氟化物的赋存和分布情况,重点介绍了火山和非火山地热系统的对比。它分析了这些水中氟化物的各种来源,并阐明了推动其动员的机制。在火山地热系统中,氟化物主要来自岩浆挥发物,而在非火山地热系统中,氟化物主要来自矿物的溶解。温度是影响地热水氟化物浓度的关键因素,碱性条件和低钙水平有利于氟化物的富集。这篇综述详细介绍了氟化物浓度如何随着地热流体从较深的地层向较浅的地层迁移而变化。根据氟化物的富集特征,探讨了地热氟化物的潜在应用前景。探讨了地热氟化物对环境的影响,介绍了各种处理方法,总结了国内外的研究现状,提出了今后的研究方向。本研究对制定合理的氟化物管理政策和制定地热资源可持续发展战略具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
Fluoride in geothermal water: Occurrence, origin, migration and environmental impact
Geothermal water, a vital renewable energy source extensively harnessed for heating and power generation, is marred by a prevalent issue – high fluoride content. The environmental impact of geothermal fluoride has been recognized globally. The natural discharge of geothermal water, coupled with its widespread exploitation, instigates the translocation of geothermal fluoride toward shallow and surface water ecosystems, culminating in escalating fluoride concentrations, thereby posing potential threats to both ecosystems and human health. Nevertheless, despite the pivotal significance of fluoride in geothermal water, a comprehensive understanding of its origins, migratory dynamics, ecological consequences, and ameliorative methodologies remains to be studied. This review provides a comprehensive examination of fluoride's global occurrence and distribution in geothermal waters, emphasizing the contrast between volcanic and non-volcanic geothermal systems. It analyzes the various sources of fluoride in these waters and elucidates the mechanisms driving its mobilization. In volcanic geothermal systems, fluoride primarily derives from magmatic volatiles, while in non-volcanic systems, it mainly results from the dissolution of minerals. Temperature is a key factor influencing fluoride concentration in geothermal waters, with alkaline conditions and low calcium levels contributing to higher fluoride enrichment. The review details how fluoride concentrations change as geothermal fluids migrate from deeper to shallower layers. Based on the enrichment characteristics of fluorides, this paper explores the potential applications of geothermal fluorides. It also examines the environmental impacts of geothermal fluoride, presents various treatment methods, and provides a summary of current research both domestically and internationally, while proposing directions for future studies. This study is instrumental in formulating judicious fluoride management policies and establishing sustainable strategies for the development of geothermal resources.
求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
Journal of Geochemical Exploration
Journal of Geochemical Exploration 地学-地球化学与地球物理
CiteScore
7.40
自引率
7.70%
发文量
148
审稿时长
8.1 months
期刊介绍: Journal of Geochemical Exploration is mostly dedicated to publication of original studies in exploration and environmental geochemistry and related topics. Contributions considered of prevalent interest for the journal include researches based on the application of innovative methods to: define the genesis and the evolution of mineral deposits including transfer of elements in large-scale mineralized areas. analyze complex systems at the boundaries between bio-geochemistry, metal transport and mineral accumulation. evaluate effects of historical mining activities on the surface environment. trace pollutant sources and define their fate and transport models in the near-surface and surface environments involving solid, fluid and aerial matrices. assess and quantify natural and technogenic radioactivity in the environment. determine geochemical anomalies and set baseline reference values using compositional data analysis, multivariate statistics and geo-spatial analysis. assess the impacts of anthropogenic contamination on ecosystems and human health at local and regional scale to prioritize and classify risks through deterministic and stochastic approaches. Papers dedicated to the presentation of newly developed methods in analytical geochemistry to be applied in the field or in laboratory are also within the topics of interest for the journal.
期刊最新文献
Insights into the mineralogy and distribution of Co, Ni, As and Bi in the sediment-hosted polymetallic ores of the Kupferschiefer in Lusatia, Germany Genetic discrimination of the Dongshan Pb-Zn-Cu deposit based on sphalerite chemistry Mineralogical and geochemical analysis of the Benjamin River South Cu-Mo-Au porphyry system in northeastern New Brunswick, Canada: A fertile adakitic magmatic system linked to slab failure Origin and migration of ore-forming fluids in the Dafulou tin deposit, Dachang district, South China: Constraints from cassiterite UPb geochronology, trace elements, fluid inclusions and oxygen isotopes In situ apatite fission track, UPb and trace elements analysis using LA-ICP-MS
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1