Titlebook: Water Resources and Integrated Management of the United Arab Emirates; Abdulrahman S. Alsharhan,Zeinelabidin E. Rizk Book 2020 Springer Na

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Ophiolite Aquiferaquifers separated by an aquiclude..The upper aquifer has a variable thickness, increasing from 60?m, at the foothills of the eastern mountain ranges, to 160 m in a northwest–southeast trending trough. The aquifer trough is composed of gravel of the Neogene age and has minor marl and sandstone inter

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Liwa Quaternary Sand Aquiferinat Zayed, and another small elliptical mound, with an average diameter of 40?km, occurs between Bu Hasa and Habshan areas. In Liwa, the groundwater depth is <5 to >50?m, and in Bu Hasa the groundwater depth is 24–52 m. The aquifer’s hydraulic parameters are: “hydraulic conductivity (K) is 2.3–8.5?

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