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- The majority of the Quaternary aquifer in Wadi Fatimah basin was represented as low-to-moderately vulnerable zones (64%, i.e., protected areas). A small portion of the aquifer in the upstream of the Wadi was identified as the very highest vulnerable zone (about 4.7%).
www.researchgate.net/publication/360029745_Groundwater_evolution_and_vulnerability_in_semi-arid_regions_using_modeling_and_GIS_tools_for_sustainable_development_case_study_of_Wadi_Fatimah_Saudi_ArabiaGroundwater evolution and vulnerability in semi-arid regions ...
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How vulnerable is Wadi Fatimah aquifer?
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Apr 18, 2022 · The majority of the Quaternary aquifer in Wadi Fatimah basin was represented as low-to-moderately vulnerable zones (64%, i.e., protected areas). A small portion of the aquifer in the upstream of the Wadi was identified as the very highest vulnerable zone (about 4.7%).
The majority of the Quaternary aquifer in Wadi Fatimah basin was represented as low-to-moderately vulnerable zones (64%, i.e., protected areas). A small portion of the aquifer in the...
Mar 8, 2003 · The majority of the Quaternary aquifer in Wadi Fatimah basin was represented as low-to-moderately vulnerable zones (64%, i.e., protected areas).
Dec 1, 2023 · Abstract. This research aims at determining and analysing the causes and consequences of desertification in the middle zone of Wadi Fatimah using satellite images, climatic data, and topographic maps.
Saudi Arabia is one of the region’s largest consumers of water, so it is important to take immediate action to address this issue. This study used data from the Gravity Recovery and Climate Experiment (GRACE) to assess changes in groundwater storage in Wadi Fatimah and its surrounding areas.
Mar 30, 2023 · The DEM and slope maps indicate that Wadi Fatimah has a high potential to store great amounts of groundwater. The maximum elevations range from 0 to 933 m, with an average elevation of 466 m AMSL. The amount of surface water that infiltrates into the ground is affected by the slope.
Apr 5, 2012 · In the different sub-basins of Wadi Fatimah, volcaniclastic sediments of Fatimah Formation, basalts and andesites of the lower member of Fatimah Formation, and Gabbros are the major sources of Na, Ca 2+, Mg 2+, Fe 2+, and K +.
