进步 发表于 2025-4-1 01:54:58
http://reply.papertrans.cn/103/10211/1021034/1021034_61.pngCalculus 发表于 2025-4-1 06:46:19
http://reply.papertrans.cn/103/10211/1021034/1021034_62.png发酵剂 发表于 2025-4-1 12:11:09
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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罗盘 发表于 2025-4-1 20:30:45
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克制 发表于 2025-4-2 00:57:35
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 declCIS 发表于 2025-4-2 05:50:01
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熄灭 发表于 2025-4-2 08:42:53
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http://reply.papertrans.cn/103/10211/1021034/1021034_69.png高兴一回 发表于 2025-4-2 18:20:23
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