Nahar Mst Shamsun, Zhang Jing, Ueda Akira, Yoshihisa Fujishiro
Department of Environmental Biology and Chemistry, Graduate School of Science and Engineering, University of Toyama, 3190 Gofuku, Toyama, 930-8555, Japan,
Environ Geochem Health. 2014 Dec;36(6):1079-94. doi: 10.1007/s10653-014-9616-5. Epub 2014 Apr 19.
The present study evaluated water supply geochemistry in Dhaka City, Bangladesh, to provide detailed trace level (subppb) water quality data that include major ions, low dissolved oxygen (DO) and toxic trace metals for sustainable development. Dhaka Groundwater, which almost uniformly meets the World Health Organization guideline, has become the preferred source. Due to groundwater depletion and an ever-increasing need to meet water demands by city residents, Dhaka water supply and sewerage authority has initiated the treatment of river water, despite the fact that very little is known about the geochemical structure, and trace metal content in the Dhaka water supply. Major ion composition of water samples was determined, and the results used to generate Stiff diagrams. The diagrams served to visually compare water from different sources based on units of mass/volume. Hydrochemical facies analysis showed supply ground and surface waters are comprised predominately of Ca-Na-Mg-HCO3 and Ca-Na-Mg-HCO3-Cl types. Spatial distribution of ions, and Na/Cl and Na/SiO2 molar ratio indicated that silicate weathering is the dominant geochemical process. Chemical data revealed that toxic Cr metal mobilization is associated with chemical hazards from the leather industry. The vulnerability of deep wells to contamination by As is governed by the geometry of induced groundwater flow paths and the geochemical conditions encountered between the shallow and deep regions of the aquifer. Quantifying total arsenic (As) and As from interlocking geochemical cycles (Fe, Mn) may assist in interpreting As dynamics in Dhaka well water. The surface source water was hypoxic to anoxic low DO associated with very high concentrations of biological oxygen demands, and electrical conductivity compared to industrial and non-industrial urban processes and standard activity guidelines. The results of this study should be applied to future research focused on the potential to improve water quality in urban and surrounding areas.
本研究评估了孟加拉国达卡市的供水地球化学,以提供详细的痕量水平(亚微克/升)水质数据,包括主要离子、低溶解氧(DO)和有毒痕量金属,以促进可持续发展。几乎完全符合世界卫生组织准则的达卡地下水已成为首选水源。由于地下水枯竭以及城市居民对满足用水需求的需求不断增加,达卡供水和排水管理局已开始对河水进行处理,尽管对达卡供水的地球化学结构和痕量金属含量了解甚少。测定了水样的主要离子组成,并将结果用于生成施蒂夫图。这些图用于根据质量/体积单位直观地比较不同水源的水。水化学相分析表明,供应的地表水和地下水主要由Ca-Na-Mg-HCO3和Ca-Na-Mg-HCO3-Cl类型组成。离子的空间分布以及Na/Cl和Na/SiO2摩尔比表明,硅酸盐风化是主要的地球化学过程。化学数据显示,有毒的铬金属迁移与皮革行业的化学危害有关。深井对砷污染的脆弱性受诱导地下水流路径的几何形状以及含水层浅层和深层之间遇到的地球化学条件的控制。量化来自相互关联的地球化学循环(铁、锰)中的总砷(As)和砷,可能有助于解释达卡井水的砷动态。地表水源水处于缺氧至厌氧的低溶解氧状态,与非常高的生物需氧量以及与工业和非工业城市过程及标准活性指南相比的电导率有关。本研究结果应应用于未来关注改善城市及周边地区水质潜力的研究。