Interpreting hydrogeochemical interactions and controlling processes in groundwater using advanced statistical techniques in the Southeast Asian megacity: Dhaka, Bangladesh

Mahir Tajwar , Mahfuzur Rahman , Mahmudul Hasan , Nazmus Sakib , Shamiha Shafinaz Shreya , Mir Md Tasnim Alam , Md. Yousuf Gazi , Sharaf Anika Hoque , Anwar Zahid
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Abstract

Groundwater quality is under increasing threat in rapidly urbanizing Southeast Asian megacities, where unregulated expansion and industrial activity are altering subsurface geochemical conditions. In Dhaka, Bangladesh, groundwater serves as a crucial source of potable water for millions, necessitating rigorous assessment of its suitability for human and agricultural use. This research seeks to comprehensively assess the hydrogeochemical characteristics of shallow groundwater, evaluating its suitability for both drinking and irrigation purposes using a combined approach of geochemical methods, multivariate statistical analyses, and geospatial techniques. The hydrogeochemical analysis of 15 groundwater samples revealed a cation order of Ca2 + > Na+ > Mg2+ > K+ and an anion order of HCO3 > Cl > SO42− > NO3. The primary objective of this research is to assess the hydrogeochemical characteristics and water quality of shallow groundwater in Dhaka using a combination of graphical techniques, multivariate statistical analyses, and water quality indices. Fifteen groundwater samples were collected during the dry season and analyzed for major cations and anions. Piper, Gibbs, Durov, and Stiff diagrams were employed to identify dominant processes. Principal Component Analysis (PCA) and hierarchical clustering were used to distinguish geogenic and anthropogenic influences. Results revealed that groundwater is dominated by the calcium bicarbonate type, with cation order Ca²⁺ > Na⁺ > Mg²⁺ > K⁺ and anion order HCO₃⁻ > Cl⁻ > SO₄²⁻ > NO₃⁻. Cation exchange and silicate weathering were identified as the significant processes influencing water chemistry. PCA revealed that three principal components accounted for 86.4 % of the variance, indicating the influence of both natural mineral dissolution and localized anthropogenic inputs. According to the Water Quality Index (WQI), 5 samples were excellent, 6 were good, and 4 were poor for drinking purposes. All samples were suitable for irrigation based on SAR, RSC, SSP, EC, and TDS values. These findings provide a robust baseline for groundwater quality monitoring in Dhaka and similar urban areas. The integrated methodology can guide policy decisions on water resource protection and help communities prioritize safe groundwater use for both domestic and agricultural needs. The study offers valuable information for assessing water quality, monitoring contamination risks, and developing groundwater management strategies, particularly in rapidly urbanizing regions of Southeast Asia.
利用先进的统计技术解释东南亚特大城市:孟加拉国达卡的水文地球化学相互作用和地下水控制过程
在快速城市化的东南亚特大城市中,地下水质量受到越来越大的威胁,这些城市不受管制的扩张和工业活动正在改变地下地球化学条件。在孟加拉国的达卡,地下水是数百万人饮用水的重要来源,需要对其是否适合人类和农业使用进行严格评估。本研究旨在综合评价浅层地下水的水文地球化学特征,利用地球化学方法、多元统计分析和地理空间技术相结合的方法评估其饮用和灌溉的适宜性。15个地下水样品的水文地球化学分析显示,阳离子顺序为Ca2 + >;Na +比;Mg2 +比;K+和HCO3−>; Cl−>; SO42−>; NO3−的阴离子顺序。本研究的主要目的是利用图形技术、多元统计分析和水质指数相结合的方法评估达卡浅层地下水的水文地球化学特征和水质。在旱季收集了15个地下水样本,分析了主要的阳离子和阴离子。使用Piper, Gibbs, Durov和Stiff图来确定主导过程。采用主成分分析(PCA)和层次聚类方法区分地质和人为影响。结果表明,地下水以碳酸钙型为主,阳离子型的Ca 2 + >; Na + >; Mg 2 + >; K +和阴离子型的HCO₃⁻>; Cl⁻>; SO₄²⁻>; NO₃⁻。阳离子交换和硅酸盐风化是影响水化学的重要过程。主成分分析结果表明,3个主成分占86.4 %的方差,表明自然矿物溶解和局部人为输入的影响。根据水质指数(WQI), 5个样本为优,6个为良,4个为差。根据SAR、RSC、SSP、EC和TDS值,所有样品都适合灌溉。这些发现为达卡和类似城市地区的地下水质量监测提供了可靠的基线。综合方法可以指导有关水资源保护的政策决定,并帮助社区优先考虑满足家庭和农业需要的地下水安全使用。这项研究为评估水质、监测污染风险和制定地下水管理战略提供了有价值的信息,特别是在快速城市化的东南亚地区。
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