Groundwater’s seasonal variation and its impact on freshwater in a coastal mega city

IF 2.8 4区 环境科学与生态学 Q3 ENVIRONMENTAL SCIENCES Environmental Earth Sciences Pub Date : 2025-02-11 DOI:10.1007/s12665-025-12092-9
Simu Akter, Mst. Sanzida Jahan Sharna, Eshrat Zahan Eshita, Md. Tanjim Hasan
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Abstract

A comprehensive groundwater quality assessment is carried out in Khulna, which is the coastal mega city of Bangladesh adjacent to southwest Bengal delta. The study was conducted to identify the seasonal variation of ion composition in groundwater and insight into its impact on freshwater availability for the study area. Results of chemical analysis revealed that groundwater is alkaline, with dominant ion concentrations of Mg2+, Na+, Cl and HCO3. Cl concentration (254.70 mg/L in monsoon; 478 mg/L in winter; 531.75 mg/L in summer) exceed from the prescribed limits, i.e., 250 mg/L of WHO water quality standards. The Piper diagram indicated that groundwater occupies saline and mixed zone that are mostly affected by the seawater through ion exchange mechanism. The Endmember diagrams revealed that silicate weathering plays a major role while evaporite dissolution and carbonate weathering play the minor role for the evolution of groundwater. Saturation indexes reveal that halite saturation increases proportionally to Cl contents while calcite saturation shows most of the groundwater samples are undersaturated. WQI revealed that summer groundwater quality is poor for drinking purposes. Furthermore, the spatial distribution map of WQI indicated that the northeast and southwest parts of groundwater are vulnerable owing to landscape dynamics. The feedback and outlooks of seasonal ion concentration on freshwater indicated suitable water quality in monsoon and winter, whereas unsuitable, salty and hard water in the summer.

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库尔纳是孟加拉国的沿海大城市,毗邻孟加拉湾三角洲西南部。这项研究旨在确定地下水中离子组成的季节性变化,并深入了解其对研究地区淡水供应的影响。化学分析结果显示,地下水呈碱性,主要离子浓度为 Mg2+、Na+、Cl- 和 HCO3-。Cl- 浓度(季风季节为 254.70 毫克/升;冬季为 478 毫克/升;夏季为 531.75 毫克/升)超过了规定的限度,即世界卫生组织水质标准的 250 毫克/升。Piper 图显示,地下水位于盐碱地和混合区,主要通过离子交换机制受到海水的影响。Endmember 图显示,硅酸盐风化对地下水的演变起主要作用,而蒸发岩溶解和碳酸盐风化则起次要作用。饱和度指数显示,海绿石饱和度与 Cl- 含量成正比增加,而方解石饱和度则显示大多数地下水样本处于不饱和状态。水质指数显示,夏季地下水水质较差,不适合饮用。此外,水质指数的空间分布图显示,由于地貌动态变化,地下水的东北部和西南部易受影响。淡水季节性离子浓度的反馈和展望表明,季风季节和冬季水质适宜,而夏季水质不适宜、偏咸和偏硬。
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来源期刊
Environmental Earth Sciences
Environmental Earth Sciences 环境科学-地球科学综合
CiteScore
5.10
自引率
3.60%
发文量
494
审稿时长
8.3 months
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.
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