Deize Elle Ribeiro Moitinho , Natanael da Silva Barbosa , David Debruyne , Maria da Conceição Rabelo Gomes , Natali Barbosa , Ludimilla Amorim Gomes , José Carlos Cruz do Carmo , Cristovaldo Bispo dos Santos
{"title":"解读巴西 Ilhas-São Sebastião 多层含水层系统的水文地球化学演变:对地下水资源管理的影响","authors":"Deize Elle Ribeiro Moitinho , Natanael da Silva Barbosa , David Debruyne , Maria da Conceição Rabelo Gomes , Natali Barbosa , Ludimilla Amorim Gomes , José Carlos Cruz do Carmo , Cristovaldo Bispo dos Santos","doi":"10.1016/j.gsd.2024.101253","DOIUrl":null,"url":null,"abstract":"<div><p>This study examines the hydrogeochemical processes shaping groundwater quality in the Ilhas-São Sebastião aquifer system, situated at the interface of the Central and Southern Recôncavo basins in the densely populated area near the Brazilian metropolis Salvador. Analysis of 71 groundwater samples reveals distinctive hydrogeochemical compositions in aquifers. In the São Sebastião aquifer, alkalis (Na<sup>+</sup> + K<sup>+</sup>) and strong acids (Cl<sup>−</sup> and SO<sub>4</sub><sup>2−</sup>) prevail. Furthermore, a moderate correlation of Na+–Cl-marks an evolution from Mg–Ca–HCO3 to Mg–Ca–Cl and Na–Cl facies. In contrast, the Ilhas aquifer displays a Na<sup>+</sup>>Ca<sup>2</sup>+>Mg<sup>2+</sup>>K<sup>+</sup> relationship for cations and HCO<sub>3</sub><sup>−</sup> > Cl<sup>−</sup> > SO<sub>4</sub><sup>2−</sup> > CO<sub>3</sub><sup>2−</sup> for anions and a recharge-discharge trajectory from the Mg–Ca–HCO<sub>3</sub> to the Ca–Na–HCO<sub>3</sub> facies. Additionally, it presents greater mineralization and dispersion of physicochemical parameters, especially around sub-basin depocenters. Its hydrogeochemical signature is characterized by robust correlations between TDS and EC, and between these parameters and SO<sub>4</sub><sup>2−</sup>, HCO<sub>3</sub><sup>−</sup>, Ca<sup>2+</sup>, and Mg<sup>2+</sup>, complemented by moderate correlations of EC with Na<sup>+</sup> and Cl<sup>−</sup>. Bivariate Gibbs diagrams and ionic ratios indicate silicate weathering and ion exchange as the primary geochemical processes controlling solute concentrations in both aquifers. However, in the Ilhas aquifer, a subordinate contribution from reverse ion exchange is indicated by weak (TDS–Na<sup>+</sup>, TDS–K<sup>+</sup>, Na<sup>+</sup>–Ca<sup>2+</sup>, K<sup>+</sup>–Ca<sup>2+</sup>) and positive TDS–Ca<sup>2+</sup> and TDS–Mg<sup>2+</sup> correlations. Conversely, negative chloroalkaline indices and the moderate Na<sup>+</sup>–Cl<sup>-</sup> correlation indicate that reverse ion exchange processes are mostly absent in the São Sebastião aquifer. Instead, both chloroalkaline imbalance reactions and silicate weathering contribute equally to the observed geochemical patterns. Groundwater geochemical signatures indicate recharge on flexural margins, active water-rock interaction in large depocenters, and mixing of hydrogeochemical facies between aquifer units. These insights contribute to a comprehensive understanding of groundwater evolution, crucial for effective water resource management in the region.</p></div>","PeriodicalId":37879,"journal":{"name":"Groundwater for Sustainable Development","volume":null,"pages":null},"PeriodicalIF":4.9000,"publicationDate":"2024-06-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Deciphering hydrogeochemical evolution in the multilayered Ilhas-São Sebastião aquifer system, Brazil: Implications for groundwater resources management\",\"authors\":\"Deize Elle Ribeiro Moitinho , Natanael da Silva Barbosa , David Debruyne , Maria da Conceição Rabelo Gomes , Natali Barbosa , Ludimilla Amorim Gomes , José Carlos Cruz do Carmo , Cristovaldo Bispo dos Santos\",\"doi\":\"10.1016/j.gsd.2024.101253\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>This study examines the hydrogeochemical processes shaping groundwater quality in the Ilhas-São Sebastião aquifer system, situated at the interface of the Central and Southern Recôncavo basins in the densely populated area near the Brazilian metropolis Salvador. Analysis of 71 groundwater samples reveals distinctive hydrogeochemical compositions in aquifers. In the São Sebastião aquifer, alkalis (Na<sup>+</sup> + K<sup>+</sup>) and strong acids (Cl<sup>−</sup> and SO<sub>4</sub><sup>2−</sup>) prevail. Furthermore, a moderate correlation of Na+–Cl-marks an evolution from Mg–Ca–HCO3 to Mg–Ca–Cl and Na–Cl facies. In contrast, the Ilhas aquifer displays a Na<sup>+</sup>>Ca<sup>2</sup>+>Mg<sup>2+</sup>>K<sup>+</sup> relationship for cations and HCO<sub>3</sub><sup>−</sup> > Cl<sup>−</sup> > SO<sub>4</sub><sup>2−</sup> > CO<sub>3</sub><sup>2−</sup> for anions and a recharge-discharge trajectory from the Mg–Ca–HCO<sub>3</sub> to the Ca–Na–HCO<sub>3</sub> facies. Additionally, it presents greater mineralization and dispersion of physicochemical parameters, especially around sub-basin depocenters. Its hydrogeochemical signature is characterized by robust correlations between TDS and EC, and between these parameters and SO<sub>4</sub><sup>2−</sup>, HCO<sub>3</sub><sup>−</sup>, Ca<sup>2+</sup>, and Mg<sup>2+</sup>, complemented by moderate correlations of EC with Na<sup>+</sup> and Cl<sup>−</sup>. Bivariate Gibbs diagrams and ionic ratios indicate silicate weathering and ion exchange as the primary geochemical processes controlling solute concentrations in both aquifers. However, in the Ilhas aquifer, a subordinate contribution from reverse ion exchange is indicated by weak (TDS–Na<sup>+</sup>, TDS–K<sup>+</sup>, Na<sup>+</sup>–Ca<sup>2+</sup>, K<sup>+</sup>–Ca<sup>2+</sup>) and positive TDS–Ca<sup>2+</sup> and TDS–Mg<sup>2+</sup> correlations. Conversely, negative chloroalkaline indices and the moderate Na<sup>+</sup>–Cl<sup>-</sup> correlation indicate that reverse ion exchange processes are mostly absent in the São Sebastião aquifer. Instead, both chloroalkaline imbalance reactions and silicate weathering contribute equally to the observed geochemical patterns. Groundwater geochemical signatures indicate recharge on flexural margins, active water-rock interaction in large depocenters, and mixing of hydrogeochemical facies between aquifer units. These insights contribute to a comprehensive understanding of groundwater evolution, crucial for effective water resource management in the region.</p></div>\",\"PeriodicalId\":37879,\"journal\":{\"name\":\"Groundwater for Sustainable Development\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":4.9000,\"publicationDate\":\"2024-06-28\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Groundwater for Sustainable Development\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S2352801X24001760\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"ENGINEERING, ENVIRONMENTAL\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Groundwater for Sustainable Development","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S2352801X24001760","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ENGINEERING, ENVIRONMENTAL","Score":null,"Total":0}
Deciphering hydrogeochemical evolution in the multilayered Ilhas-São Sebastião aquifer system, Brazil: Implications for groundwater resources management
This study examines the hydrogeochemical processes shaping groundwater quality in the Ilhas-São Sebastião aquifer system, situated at the interface of the Central and Southern Recôncavo basins in the densely populated area near the Brazilian metropolis Salvador. Analysis of 71 groundwater samples reveals distinctive hydrogeochemical compositions in aquifers. In the São Sebastião aquifer, alkalis (Na+ + K+) and strong acids (Cl− and SO42−) prevail. Furthermore, a moderate correlation of Na+–Cl-marks an evolution from Mg–Ca–HCO3 to Mg–Ca–Cl and Na–Cl facies. In contrast, the Ilhas aquifer displays a Na+>Ca2+>Mg2+>K+ relationship for cations and HCO3− > Cl− > SO42− > CO32− for anions and a recharge-discharge trajectory from the Mg–Ca–HCO3 to the Ca–Na–HCO3 facies. Additionally, it presents greater mineralization and dispersion of physicochemical parameters, especially around sub-basin depocenters. Its hydrogeochemical signature is characterized by robust correlations between TDS and EC, and between these parameters and SO42−, HCO3−, Ca2+, and Mg2+, complemented by moderate correlations of EC with Na+ and Cl−. Bivariate Gibbs diagrams and ionic ratios indicate silicate weathering and ion exchange as the primary geochemical processes controlling solute concentrations in both aquifers. However, in the Ilhas aquifer, a subordinate contribution from reverse ion exchange is indicated by weak (TDS–Na+, TDS–K+, Na+–Ca2+, K+–Ca2+) and positive TDS–Ca2+ and TDS–Mg2+ correlations. Conversely, negative chloroalkaline indices and the moderate Na+–Cl- correlation indicate that reverse ion exchange processes are mostly absent in the São Sebastião aquifer. Instead, both chloroalkaline imbalance reactions and silicate weathering contribute equally to the observed geochemical patterns. Groundwater geochemical signatures indicate recharge on flexural margins, active water-rock interaction in large depocenters, and mixing of hydrogeochemical facies between aquifer units. These insights contribute to a comprehensive understanding of groundwater evolution, crucial for effective water resource management in the region.
期刊介绍:
Groundwater for Sustainable Development is directed to different stakeholders and professionals, including government and non-governmental organizations, international funding agencies, universities, public water institutions, public health and other public/private sector professionals, and other relevant institutions. It is aimed at professionals, academics and students in the fields of disciplines such as: groundwater and its connection to surface hydrology and environment, soil sciences, engineering, ecology, microbiology, atmospheric sciences, analytical chemistry, hydro-engineering, water technology, environmental ethics, economics, public health, policy, as well as social sciences, legal disciplines, or any other area connected with water issues. The objectives of this journal are to facilitate: • The improvement of effective and sustainable management of water resources across the globe. • The improvement of human access to groundwater resources in adequate quantity and good quality. • The meeting of the increasing demand for drinking and irrigation water needed for food security to contribute to a social and economically sound human development. • The creation of a global inter- and multidisciplinary platform and forum to improve our understanding of groundwater resources and to advocate their effective and sustainable management and protection against contamination. • Interdisciplinary information exchange and to stimulate scientific research in the fields of groundwater related sciences and social and health sciences required to achieve the United Nations Millennium Development Goals for sustainable development.