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

IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Groundwater for Sustainable Development Pub Date : 2024-06-28 DOI:10.1016/j.gsd.2024.101253
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
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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>&gt;Ca<sup>2</sup>+&gt;Mg<sup>2+</sup>&gt;K<sup>+</sup> relationship for cations and HCO<sub>3</sub><sup>−</sup> &gt; Cl<sup>−</sup> &gt; SO<sub>4</sub><sup>2−</sup> &gt; 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>. 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引用次数: 0

摘要

本研究探讨了影响 Ilhas-São Sebastião 含水层系统地下水质量的水文地质化学过程,该含水层系统位于巴西大都市萨尔瓦多附近人口稠密地区中部和南部雷孔卡沃盆地的交界处。对 71 个地下水样本的分析表明,含水层的水文地质化学成分各不相同。在圣塞巴斯蒂昂含水层中,碱(Na+ + K+)和强酸(Cl- 和 SO42-)占主导地位。此外,Na+-Cl 的适度相关性标志着从 Mg-Ca-HCO3 到 Mg-Ca-Cl 和 Na-Cl 层的演变。相比之下,伊尔哈斯含水层的阳离子与 HCO3- > Cl- > SO42- > CO32- 呈 Na+>Ca2+>Mg2+>K+关系,阴离子则从 Mg-Ca-HCO3 到 Ca-Na-HCO3 层的补给-排泄轨迹。此外,它的矿化度更高,物理化学参数更分散,尤其是在次盆地沉积中心周围。其水文地质化学特征是 TDS 与 EC 之间以及这些参数与 SO42-、HCO3-、Ca2+ 和 Mg2+ 之间的强相关性,以及 EC 与 Na+ 和 Cl- 的中度相关性。双变量吉布斯图和离子比率表明,硅酸盐风化和离子交换是控制两个含水层溶质浓度的主要地球化学过程。然而,在伊尔哈斯含水层中,反向离子交换的作用次之,表现为微弱的(TDS-Na+、TDS-K+、Na+-Ca2+、K+-Ca2+)和正的 TDS-Ca2+ 和 TDS-Mg2+ 关联。相反,负的氯碱指数和适度的 Na+-Cl- 相关性表明,圣塞巴斯蒂昂含水层大多不存在反向离子交换过程。相反,氯碱失衡反应和硅酸盐风化作用对观察到的地球化学模式起着同等作用。地下水地球化学特征显示了挠曲边缘的补给、大型沉积中心活跃的水岩相互作用以及含水层单元之间水文地球化学面貌的混合。这些见解有助于全面了解地下水的演变,对该地区有效的水资源管理至关重要。
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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.

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来源期刊
Groundwater for Sustainable Development
Groundwater for Sustainable Development Social Sciences-Geography, Planning and Development
CiteScore
11.50
自引率
10.20%
发文量
152
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.
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