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Abstract: In the temperate and semiarid environment the salinity of both surface and subsurface(meteoric) waters is dominated by the weathering products of soil and aquifer minerals, since even surface waters have a history of subsurface flow. In the desert environment, in contrast, surface flows are more superficial and their chemistry dominated by the aeolian salinity. This has both a marine input and
a contribution from recycled salinity from surface accumulation of evaporitic minerals. Both these sources have chloride (and to a lesser extent sulphate) as the dominant anion.
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Gaye, C. B. (2001). Isotope techniques for monitoring groundwater salinization. Hydrogeology Journal, 9, 217–218.
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Ghabayen, S., McKee, M., & Kemblowski, M. (2006). Ionic and Isotopic Ratios for Identification of Salinity Sources and Missing Data in the Gaza Aquifer. Journal of Hydrology, 318, 360–373.
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