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Sources of deep groundwater salinity in the southwestern zone of Bangladesh
Authors:Mirza A T M Tanvir Rahman  Ratan Kumar Majumder  Syed Hafizur Rahman  Md Abdul Halim
Institution:(1) Department of Environmental Sciences, Jahangirnagar University, Savar, Dhaka, Bangladesh;(2) Institute of Nuclear Science and Technology, AERE, Savar, GPO Box 3787, Dhaka, 1000, Bangladesh;
Abstract:Twenty groundwater samples were collected from two different areas in Satkhira Sadar Upazila to identify the source of salinity in deep groundwater aquifer. Most of the analyzed groundwater is of Na–Cl–HCO3 type water. The trends of anion and cation are Cl > HCO3  > NO3  > SO4 2− and Na+ > Ca2+ > Mg2+ > K+, respectively. Groundwater chemistry in the study area is mainly governed by rock dissolution and ion exchange. The dissolved minerals in groundwater mainly come from silicate weathering. The salinity of groundwater samples varies from ~1 to ~5%, and its source is possibly the paleo-brackish water which may be entrapped during past geologic periods.
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