Mingqian Li, He Wang, Hongbiao Gu, Jiang Sun, Baoming Chi
{"title":"吉林西部地下水氟、砷区域分布控制过程评价","authors":"Mingqian Li, He Wang, Hongbiao Gu, Jiang Sun, Baoming Chi","doi":"10.1007/s12665-024-12000-7","DOIUrl":null,"url":null,"abstract":"<div><p>Groundwater is a critical resource for a locality, and high F and As contents in groundwater can substantially impact regional ecological stability. The Western Plain of Jilin has groundwater > 128 m, and F and As levels exceed the World Health Organization’s (WHO) safe drinking levels. To assess the primary processes controlling the regional distribution of F and As in the aquifer, 225 wells at varying depths were selected and analyzed for groundwater sampling in the plain. Concentration ranges of F and As in the groundwater were 0.16–7.99 and 1–310 µg/L, respectively. Approximately 33% and 20% of the samples exceeded the WHO limit for F (1.5 mg/L) and As (10 µg/L), respectively. F and As were not significantly correlated. In the central part of the plain, the groundwater upstream of the Huolin River Basin had higher As concentrations, whereas the groundwater downstream had higher F concentrations. The sources and enrichment of F and As predominantly resulted from widespread natural processes with little signs of anthropogenic influence. Regional of F and As distributions are controlled by two processes: hydrogeological controls primarily in the upstream region of the Huolin River and hydrogeochemical controls mainly occurring in the middle and downstream areas of the river. The primary hydrogeochemical processes controlling F and As distribution and migration in the study area are the dissolution of carbonate rock (where HCO<sub>3</sub><sup>−</sup> may act as a sorption competitor), an increase in pH, and cation exchange (release of Na<sup>+</sup> and adsorption of Ca<sup>2+</sup>). Evapotranspiration only influences the enrichment process of F and As concentrations in localized shallow groundwater. Human–induced groundwater extraction is the primary cause of F and As migration in medium and deep groundwater. The mixing of highly concentrated F- and As-containing groundwater with uncontaminated groundwater presents a potential problem for future research.</p></div>","PeriodicalId":542,"journal":{"name":"Environmental Earth Sciences","volume":"83 24","pages":""},"PeriodicalIF":2.8000,"publicationDate":"2024-12-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Assessment of processes controlling the regional distribution of fluoride and arsenic in groundwater of the Western Jilin Province, Northeast China\",\"authors\":\"Mingqian Li, He Wang, Hongbiao Gu, Jiang Sun, Baoming Chi\",\"doi\":\"10.1007/s12665-024-12000-7\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Groundwater is a critical resource for a locality, and high F and As contents in groundwater can substantially impact regional ecological stability. The Western Plain of Jilin has groundwater > 128 m, and F and As levels exceed the World Health Organization’s (WHO) safe drinking levels. To assess the primary processes controlling the regional distribution of F and As in the aquifer, 225 wells at varying depths were selected and analyzed for groundwater sampling in the plain. Concentration ranges of F and As in the groundwater were 0.16–7.99 and 1–310 µg/L, respectively. Approximately 33% and 20% of the samples exceeded the WHO limit for F (1.5 mg/L) and As (10 µg/L), respectively. F and As were not significantly correlated. In the central part of the plain, the groundwater upstream of the Huolin River Basin had higher As concentrations, whereas the groundwater downstream had higher F concentrations. The sources and enrichment of F and As predominantly resulted from widespread natural processes with little signs of anthropogenic influence. Regional of F and As distributions are controlled by two processes: hydrogeological controls primarily in the upstream region of the Huolin River and hydrogeochemical controls mainly occurring in the middle and downstream areas of the river. The primary hydrogeochemical processes controlling F and As distribution and migration in the study area are the dissolution of carbonate rock (where HCO<sub>3</sub><sup>−</sup> may act as a sorption competitor), an increase in pH, and cation exchange (release of Na<sup>+</sup> and adsorption of Ca<sup>2+</sup>). Evapotranspiration only influences the enrichment process of F and As concentrations in localized shallow groundwater. Human–induced groundwater extraction is the primary cause of F and As migration in medium and deep groundwater. The mixing of highly concentrated F- and As-containing groundwater with uncontaminated groundwater presents a potential problem for future research.</p></div>\",\"PeriodicalId\":542,\"journal\":{\"name\":\"Environmental Earth Sciences\",\"volume\":\"83 24\",\"pages\":\"\"},\"PeriodicalIF\":2.8000,\"publicationDate\":\"2024-12-04\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Environmental Earth Sciences\",\"FirstCategoryId\":\"93\",\"ListUrlMain\":\"https://link.springer.com/article/10.1007/s12665-024-12000-7\",\"RegionNum\":4,\"RegionCategory\":\"环境科学与生态学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"ENVIRONMENTAL SCIENCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Environmental Earth Sciences","FirstCategoryId":"93","ListUrlMain":"https://link.springer.com/article/10.1007/s12665-024-12000-7","RegionNum":4,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
Assessment of processes controlling the regional distribution of fluoride and arsenic in groundwater of the Western Jilin Province, Northeast China
Groundwater is a critical resource for a locality, and high F and As contents in groundwater can substantially impact regional ecological stability. The Western Plain of Jilin has groundwater > 128 m, and F and As levels exceed the World Health Organization’s (WHO) safe drinking levels. To assess the primary processes controlling the regional distribution of F and As in the aquifer, 225 wells at varying depths were selected and analyzed for groundwater sampling in the plain. Concentration ranges of F and As in the groundwater were 0.16–7.99 and 1–310 µg/L, respectively. Approximately 33% and 20% of the samples exceeded the WHO limit for F (1.5 mg/L) and As (10 µg/L), respectively. F and As were not significantly correlated. In the central part of the plain, the groundwater upstream of the Huolin River Basin had higher As concentrations, whereas the groundwater downstream had higher F concentrations. The sources and enrichment of F and As predominantly resulted from widespread natural processes with little signs of anthropogenic influence. Regional of F and As distributions are controlled by two processes: hydrogeological controls primarily in the upstream region of the Huolin River and hydrogeochemical controls mainly occurring in the middle and downstream areas of the river. The primary hydrogeochemical processes controlling F and As distribution and migration in the study area are the dissolution of carbonate rock (where HCO3− may act as a sorption competitor), an increase in pH, and cation exchange (release of Na+ and adsorption of Ca2+). Evapotranspiration only influences the enrichment process of F and As concentrations in localized shallow groundwater. Human–induced groundwater extraction is the primary cause of F and As migration in medium and deep groundwater. The mixing of highly concentrated F- and As-containing groundwater with uncontaminated groundwater presents a potential problem for future research.
期刊介绍:
Environmental Earth Sciences is an international multidisciplinary journal concerned with all aspects of interaction between humans, natural resources, ecosystems, special climates or unique geographic zones, and the earth:
Water and soil contamination caused by waste management and disposal practices
Environmental problems associated with transportation by land, air, or water
Geological processes that may impact biosystems or humans
Man-made or naturally occurring geological or hydrological hazards
Environmental problems associated with the recovery of materials from the earth
Environmental problems caused by extraction of minerals, coal, and ores, as well as oil and gas, water and alternative energy sources
Environmental impacts of exploration and recultivation – Environmental impacts of hazardous materials
Management of environmental data and information in data banks and information systems
Dissemination of knowledge on techniques, methods, approaches and experiences to improve and remediate the environment
In pursuit of these topics, the geoscientific disciplines are invited to contribute their knowledge and experience. Major disciplines include: hydrogeology, hydrochemistry, geochemistry, geophysics, engineering geology, remediation science, natural resources management, environmental climatology and biota, environmental geography, soil science and geomicrobiology.