<p>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 Mg<sup>2+</sup>, Na<sup>+</sup>, Cl<sup>−</sup> and HCO<sub>3</sub><sup>−</sup>. Cl<sup>−</sup> concentration (254.70&#xa0;mg/L in monsoon; 478&#xa0;mg/L in winter; 531.75&#xa0;mg/L in summer) exceed from the prescribed limits, i.e., 250&#xa0;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<sup>−</sup> 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.</p>

错误:搜索内容不能为空,请输入英文关键词
错误:关键词超出字数限制,请精简
高级检索

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

  • Simu Akter,
  • Mst. Sanzida Jahan Sharna,
  • Eshrat Zahan Eshita,
  • Md. Tanjim Hasan

摘要

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.