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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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發(fā)表于 2025-4-1 01:54:58 | 只看該作者
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發(fā)表于 2025-4-1 18:07:46 | 只看該作者
Natural Springs: Hydrogeology, Hydrogeochemistry and Therapeutic Value the discharge rates of the Maddab and Bu Sukhanah springs are not directly related to rainfall intensity..Heavy groundwater exploitation during the period 1984–1991 appears to be the main cause of the increasing salinity of springs water, however, the increase of the salinity of the Bu Sukhanah spr
65#
發(fā)表于 2025-4-1 20:30:45 | 只看該作者
Seasonal Floods: Harvesting and Contribution to Aquifers’ Rechargef wadi Al Bih is larger than Wadi Tawiyean and Wadi Ham, the volume of surface runoff in wadi Al Bih resulting from the same rainstorm was twice the surface runoff on Wadi Ham and Wadi Tawiyean..Based on an annual average rainfall of 115?mm/year, a weighted average runoff coefficient (%) of 7.63, an
66#
發(fā)表于 2025-4-2 00:57:35 | 只看該作者
Aflaj Systems: History and Factors Affecting Recharge and Dischargeunt of recharge are the main factors affecting aflaj discharge. Aflaj systems were classified based on source of recharge and discharge into Al Gheli, Al Daudi and Al Hadouri. During the last three decades, several aflaj systems faced challenges such as excessive groundwater pumping and a sharp decl
67#
發(fā)表于 2025-4-2 05:50:01 | 只看該作者
Natural Springs: Hydrogeology, Hydrogeochemistry and Therapeutic Value the discharge rates of the Maddab and Bu Sukhanah springs are not directly related to rainfall intensity..Heavy groundwater exploitation during the period 1984–1991 appears to be the main cause of the increasing salinity of springs water, however, the increase of the salinity of the Bu Sukhanah spr
68#
發(fā)表于 2025-4-2 08:42:53 | 只看該作者
69#
發(fā)表于 2025-4-2 14:35:52 | 只看該作者
70#
發(fā)表于 2025-4-2 18:20:23 | 只看該作者
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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