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21#
發(fā)表于 2025-3-25 03:46:27 | 只看該作者
22#
發(fā)表于 2025-3-25 09:19:23 | 只看該作者
Groundwater Modelling and Assessment Under Uncertain Hydrological Conditions for Egyptian Sahara,ed in Western Egypt and is lacking hydrogeological data. Recent development of the Egyptian Sahara is mainly due to the Nubian Sandstone Aquifer System (NSAS) as a unique source of water there. NSAS covers a great part of Egypt, Sudan, Chad and Libya and is considered as a main source of freshwater.
23#
發(fā)表于 2025-3-25 15:34:41 | 只看該作者
24#
發(fā)表于 2025-3-25 17:51:26 | 只看該作者
25#
發(fā)表于 2025-3-25 23:52:09 | 只看該作者
Joe Miemczyk,Mickey Howard,Thomas E. Johnsenhe narrow valley of the Nile comprise 5.5% of the total area of Egypt. The Nile Delta aquifer, Egypt, which is replenished directly by the Nile water, is considered another renewable resource. However, this aquifer system is in direct contact with the Mediterranean Sea from the north and the Suez Ca
26#
發(fā)表于 2025-3-26 02:17:23 | 只看該作者
27#
發(fā)表于 2025-3-26 04:52:30 | 只看該作者
https://doi.org/10.1007/978-1-4471-1007-1oduction requires the largest quantities of water, with groundwater resources providing more than 40% of all water used globally for irrigated agriculture. According to the Egyptian Ministry of Irrigation and Public Works the annual water resources in Egypt depend mainly on the Nile water (55.5?BCM)
28#
發(fā)表于 2025-3-26 11:40:19 | 只看該作者
A Brief Introduction to the GSM System,nd urban development. The main water resource in Egypt is the River Nile; Nile water alone is no longer sufficient for the increasing water requirements for the different developmental activities in Egypt due to a rapid increase in population and expected impacts of climate change especially on the
29#
發(fā)表于 2025-3-26 13:27:06 | 只看該作者
30#
發(fā)表于 2025-3-26 17:05:50 | 只看該作者
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