Berenice Gómez-Mena, Janete Morán-Ramírez, Oscar Guadalupe Almanza-Tovar, Briseida López-Álvarez, Manuel Martínez-Morales, José Alfredo Ramos-Leal
{"title":"瓦哈卡综合体含水层脆弱性评估:综合 DRASTIC 方法、TEM 和水质分析","authors":"Berenice Gómez-Mena, Janete Morán-Ramírez, Oscar Guadalupe Almanza-Tovar, Briseida López-Álvarez, Manuel Martínez-Morales, José Alfredo Ramos-Leal","doi":"10.1007/s12665-024-11983-7","DOIUrl":null,"url":null,"abstract":"<div><p>This research explores the relationship between aquifer vulnerability, water quality and agricultural and mining activities carried out in a southern portion of the Central Valleys of Oaxaca. This site is located on a shallow aquifer with an average thickness of 30 – 40 m, composed mainly of gravel, sand, clay and silt. These materials constitute the alluvial fill that is considered the main hydrogeological unit, which overlies the metamorphic basement of the Oaxacan complex, which acts as a lower limit restricting the flow of water towards deep infiltration. The study applies a comprehensive methodology, which combines several approaches: the thematic weighting of layers through the DRASTIC method, the analysis of physical–chemical parameters of 145 water samples to determine quality and contamination indices, the interpretation of geological-geophysical data obtained from 11 Transient Electromagnetic Surveys (TEM) that allowed the identification of isoresistive units associated with the geology of the area, these data were complemented with geological field work. The results show that the area dedicated to agriculture has a medium to high vulnerability, with water quality varying from slightly contaminated to highly contaminated, which translates into a moderate to high level of contamination. According to the geological-geophysical interpretation, this area is located in U2b, which presents resistivities that range between 200 and 300 Ohm.m related to alluvial deposits and conglomerates. In the mining activity area, a medium vulnerability was identified, with water quality indices varying from very contaminated to contaminated and contamination levels from moderate to high. The isoresistive unit at this site corresponds to U3, with values greater than 350 Ohm.m, associated with andesitic rocks. At the recharge sites, a low vulnerability was determined, with acceptable water quality indices and low levels of contamination.</p></div>","PeriodicalId":542,"journal":{"name":"Environmental Earth Sciences","volume":"83 24","pages":""},"PeriodicalIF":2.8000,"publicationDate":"2024-11-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Aquifer vulnerability assessment in the oaxacan complex: integrating the DRASTIC methodology, TEM, and water quality analysis\",\"authors\":\"Berenice Gómez-Mena, Janete Morán-Ramírez, Oscar Guadalupe Almanza-Tovar, Briseida López-Álvarez, Manuel Martínez-Morales, José Alfredo Ramos-Leal\",\"doi\":\"10.1007/s12665-024-11983-7\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>This research explores the relationship between aquifer vulnerability, water quality and agricultural and mining activities carried out in a southern portion of the Central Valleys of Oaxaca. This site is located on a shallow aquifer with an average thickness of 30 – 40 m, composed mainly of gravel, sand, clay and silt. These materials constitute the alluvial fill that is considered the main hydrogeological unit, which overlies the metamorphic basement of the Oaxacan complex, which acts as a lower limit restricting the flow of water towards deep infiltration. The study applies a comprehensive methodology, which combines several approaches: the thematic weighting of layers through the DRASTIC method, the analysis of physical–chemical parameters of 145 water samples to determine quality and contamination indices, the interpretation of geological-geophysical data obtained from 11 Transient Electromagnetic Surveys (TEM) that allowed the identification of isoresistive units associated with the geology of the area, these data were complemented with geological field work. The results show that the area dedicated to agriculture has a medium to high vulnerability, with water quality varying from slightly contaminated to highly contaminated, which translates into a moderate to high level of contamination. According to the geological-geophysical interpretation, this area is located in U2b, which presents resistivities that range between 200 and 300 Ohm.m related to alluvial deposits and conglomerates. In the mining activity area, a medium vulnerability was identified, with water quality indices varying from very contaminated to contaminated and contamination levels from moderate to high. The isoresistive unit at this site corresponds to U3, with values greater than 350 Ohm.m, associated with andesitic rocks. At the recharge sites, a low vulnerability was determined, with acceptable water quality indices and low levels of contamination.</p></div>\",\"PeriodicalId\":542,\"journal\":{\"name\":\"Environmental Earth Sciences\",\"volume\":\"83 24\",\"pages\":\"\"},\"PeriodicalIF\":2.8000,\"publicationDate\":\"2024-11-28\",\"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/s12665-024-11983-7\",\"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/s12665-024-11983-7","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}
Aquifer vulnerability assessment in the oaxacan complex: integrating the DRASTIC methodology, TEM, and water quality analysis
This research explores the relationship between aquifer vulnerability, water quality and agricultural and mining activities carried out in a southern portion of the Central Valleys of Oaxaca. This site is located on a shallow aquifer with an average thickness of 30 – 40 m, composed mainly of gravel, sand, clay and silt. These materials constitute the alluvial fill that is considered the main hydrogeological unit, which overlies the metamorphic basement of the Oaxacan complex, which acts as a lower limit restricting the flow of water towards deep infiltration. The study applies a comprehensive methodology, which combines several approaches: the thematic weighting of layers through the DRASTIC method, the analysis of physical–chemical parameters of 145 water samples to determine quality and contamination indices, the interpretation of geological-geophysical data obtained from 11 Transient Electromagnetic Surveys (TEM) that allowed the identification of isoresistive units associated with the geology of the area, these data were complemented with geological field work. The results show that the area dedicated to agriculture has a medium to high vulnerability, with water quality varying from slightly contaminated to highly contaminated, which translates into a moderate to high level of contamination. According to the geological-geophysical interpretation, this area is located in U2b, which presents resistivities that range between 200 and 300 Ohm.m related to alluvial deposits and conglomerates. In the mining activity area, a medium vulnerability was identified, with water quality indices varying from very contaminated to contaminated and contamination levels from moderate to high. The isoresistive unit at this site corresponds to U3, with values greater than 350 Ohm.m, associated with andesitic rocks. At the recharge sites, a low vulnerability was determined, with acceptable water quality indices and low levels of contamination.
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.