Abstract
A study of the hydrochemical facies, zonation, genesis and the trend in ground water quality of Al-Sulaibiya field was conducted. The study area is located 120 km south of Kuwait Bay. It comprises the oldest and largest water well field which produces brackish ground water from the Dammam limestone aquifer. > 1000 ground watger samples in the period 1980–1990 were analysed. The study revealed the dominance of two major water types and two genetic water types of continental and marine origin: NaCl and CaSO4 and SO4-Na and Cl-Mg respectively. It also revealed that the water is mainly of chloride-sulphate and calcium-sodium facies. The aquifer salinity which increases in the NE direction, ranges from 3500 to 8000 mg L−1. The water is very hard. The total hardness as CaCO3 ranges between 1500–3500 mg L−1. Thus, the only new finding was that the salinity and the total hardness of the aquifer have increased slightly and steadily over the period under investigation.
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Al-Ruwaih, F.M. Hydrogeochemical variation of carbonate aquifer, Al-Sulaibiya, Kuwait. Water Air Soil Pollut 90, 489–505 (1996). https://doi.org/10.1007/BF00282664
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DOI: https://doi.org/10.1007/BF00282664