El Sherbini, Ragab A., Ghazala, Hosni H. ORCID: 0000-0003-3182-0071, Ahmed, Mohammed A. ORCID: 0000-0001-5370-3779, Ibraheem, Ismael M. ORCID: 0000-0001-6228-246X, Al Ajmi, Hussain F. and Genedi, Mohamed A. ORCID: 0000-0002-1384-2456 (2025). Mapping Groundwater Potential Zones in the Widyan Basin, Al Qassim, KSA: Analytical Hierarchy Process-Based Analysis Using Sentinel-2, ASTER-DEM, and Conventional Data. Remote Sensing, 17 (5). pp. 1-24. MDPI. ISSN 2072-4292

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Identification Number:10.3390/rs17050766

Abstract

[Artikel-Nr. 766] Groundwater availability in semi-arid regions like the Widyan Basin, the Kingdom of Saudi Arabia (KSA), is a critical challenge due to climatic, topographic, and hydrological variations. The accurate identification of groundwater zones is essential for sustainable development. Therefore, this study combines remote-sensing datasets (Sentinel-2 and ASTER-DEM) with conventional data using Geographic Information System (GIS) and analytical hierarchy process (AHP) techniques to delineate groundwater potential zones (GWPZs). The basin’s geology includes Pre-Cambrian rock units of the Arabian Shield in the southwest and Cambrian–Ordovician units in the northeast, with the Saq Formation serving as the main groundwater aquifer. Six soil types were identified: Haplic and Calcic Yermosols, Calcaric Regosols, Cambic Arenosols, Orthic Solonchaks, and Lithosols. The topography varies from steep areas in the southwest and northwest to nearly flat terrain in the northeast. Hydrologically, the basin is divided into 28 sub-basins with four stream orders. Using GIS-based AHP and weighted overlay methods, the GWPZs were mapped, achieving a model consistency ratio of 0.0956. The zones were categorized as excellent (15.21%), good (40.85%), fair (43.94%), and poor (0%). The GWPZ model was validated by analyzing data from 48 water wells distributed in the study area. These wells range from fresh water to primary saline water, with water depths varying between 13.98 and 130 m. Nine wells—with an average total dissolved solids (TDS) value of 597.2 mg/L—fall within the excellent zone, twenty-one wells are categorized in the good zone, fifteen wells are classified in the fair zone, and the remaining wells fall into the poor zone, with TDS values reaching up to 2177 mg/L. The results indicate that the central zone of the study area is suitable for drilling new water wells.

Item Type: Article
Creators:
Creators
Email
ORCID
ORCID Put Code
El Sherbini, Ragab A.
UNSPECIFIED
UNSPECIFIED
UNSPECIFIED
Ghazala, Hosni H.
UNSPECIFIED
UNSPECIFIED
Ahmed, Mohammed A.
UNSPECIFIED
UNSPECIFIED
Ibraheem, Ismael M.
UNSPECIFIED
UNSPECIFIED
Al Ajmi, Hussain F.
UNSPECIFIED
UNSPECIFIED
UNSPECIFIED
Genedi, Mohamed A.
UNSPECIFIED
UNSPECIFIED
URN: urn:nbn:de:hbz:38-794496
Identification Number: 10.3390/rs17050766
Journal or Publication Title: Remote Sensing
Volume: 17
Number: 5
Page Range: pp. 1-24
Number of Pages: 1
Date: 22 February 2025
Publisher: MDPI
ISSN: 2072-4292
Language: English
Faculty: Faculty of Mathematics and Natural Sciences
Divisions: Faculty of Mathematics and Natural Sciences > Department of Geosciences > Institute for Geophysics and Meteorology
Subjects: Earth sciences
Geography and travel
['eprint_fieldname_oa_funders' not defined]: Publikationsfonds UzK
Refereed: Yes
URI: http://kups.ub.uni-koeln.de/id/eprint/79449

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