HIGHLIGHTS
SUMMARY
The ionic variation on groundwater is caused by water-rock interactions and redox_reactions during water percolation via aquifer (Yetiş et_al 2019). The limitation of surface water bodies has prompted the use of groundwater for consumption in dry and semi-arid areas (Mallick et_al 2018). To intrusion and excessive groundwater exploration, the influence of salt framing on groundwater may exacerbate water quality for consumption (Selvakumar et_al 2017). Many studies related to groundwater quality and hydrogeochemistry in the coastal area were conducted (Adimalla et_al 2018; Abu-alnaeem et_al 2018; Chotpantarat et_al 2020; Hajji et_al 2020; Huizer . . .
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