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Hydrogeological and Hydrochemical Study of the Al-Shagaya Field-F, Kuwait
Abstract The study area, Al-Shagaya Field-F, is located at the south western part of Kuwait and includes twenty-seven production water wells, tapping the Kuwait Group aquifer. The main objectives of this study were to identify the aquifer type, determine its properties, outline the geological factors and the hydrochemical processes that control the quality of the groundwater of the study area, and to assess the water quality of the Kuwait Group aquifer. Analyses of aquifer test data revealed that the Kuwait Group aquifer acts as a semi-confined to confined aquifer, with a range of transmissivity values between 103 and 1,198 $ m^{2} $/day. The initial water level ranges from 70 to 146 m (M.S.L). The estimated quantity of groundwater entering the study area is about 12,950 $ m^{3} $/day. The chemical analyses show that the groundwater of the study area is a brackish water type, with total dissolved solids ranging from 3,586 to 5,334 mg/l. The aquifer salinity increases in the direction of regional flow towards the NE. The average pH value is 7.7 and the average electrical conductivity is 5,349 μs/cm. Groundwater is highly concentrated with $ Na^{+} $, $ Ca^{2+} $, $ Cl^{-} $ and $ SO_{4} $2- and is depleted in $ HCO_{3} $- and $ Mg^{2+} $ ions. It is characterized by secondary salinity, where the alkaline earths exceed the alkalies and strong acids exceed weak acids. Three groundwater chemical types are recognized: NaCl, $ Na_{2} $$ SO_{4 } $and $ CaCl_{2} $. The NaCl water type is the most abundant in the study area. The main genetic types of water are: $ MgCl_{2} $ and $ Na_{2} $$ SO_{4} $. It is found that the groundwater is oversaturated with respect to aragonite and calcite and undersaturated with respect to anhydrite, gypsum, halite and dolomite. A comparison of the hydrochemical coefficients of $ Na^{+} $/$ Cl^{-} $, $ SO_{4} $2-/$ Cl^{-} $ and $ Ca^{2+} $/$ Mg^{2+} $ in the study area with those of seawater and river water shows that the groundwater of the study area is a mixture of marine and continental water.
Hydrogeological and Hydrochemical Study of the Al-Shagaya Field-F, Kuwait
Abstract The study area, Al-Shagaya Field-F, is located at the south western part of Kuwait and includes twenty-seven production water wells, tapping the Kuwait Group aquifer. The main objectives of this study were to identify the aquifer type, determine its properties, outline the geological factors and the hydrochemical processes that control the quality of the groundwater of the study area, and to assess the water quality of the Kuwait Group aquifer. Analyses of aquifer test data revealed that the Kuwait Group aquifer acts as a semi-confined to confined aquifer, with a range of transmissivity values between 103 and 1,198 $ m^{2} $/day. The initial water level ranges from 70 to 146 m (M.S.L). The estimated quantity of groundwater entering the study area is about 12,950 $ m^{3} $/day. The chemical analyses show that the groundwater of the study area is a brackish water type, with total dissolved solids ranging from 3,586 to 5,334 mg/l. The aquifer salinity increases in the direction of regional flow towards the NE. The average pH value is 7.7 and the average electrical conductivity is 5,349 μs/cm. Groundwater is highly concentrated with $ Na^{+} $, $ Ca^{2+} $, $ Cl^{-} $ and $ SO_{4} $2- and is depleted in $ HCO_{3} $- and $ Mg^{2+} $ ions. It is characterized by secondary salinity, where the alkaline earths exceed the alkalies and strong acids exceed weak acids. Three groundwater chemical types are recognized: NaCl, $ Na_{2} $$ SO_{4 } $and $ CaCl_{2} $. The NaCl water type is the most abundant in the study area. The main genetic types of water are: $ MgCl_{2} $ and $ Na_{2} $$ SO_{4} $. It is found that the groundwater is oversaturated with respect to aragonite and calcite and undersaturated with respect to anhydrite, gypsum, halite and dolomite. A comparison of the hydrochemical coefficients of $ Na^{+} $/$ Cl^{-} $, $ SO_{4} $2-/$ Cl^{-} $ and $ Ca^{2+} $/$ Mg^{2+} $ in the study area with those of seawater and river water shows that the groundwater of the study area is a mixture of marine and continental water.
Hydrogeological and Hydrochemical Study of the Al-Shagaya Field-F, Kuwait
Al-Ruwaih, F. M. (author) / Ben-Essa, S. A. (author)
2004
Article (Journal)
English
Hydrogeological and Hydrochemical Study of the Al-Shagaya Field-F, Kuwait
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