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ORIGINAL RESEARCH article

Front. Earth Sci.
Sec. Geoscience and Society
Volume 12 - 2024 | doi: 10.3389/feart.2024.1456055

Integrated approach-based groundwater mapping in Sohag Governorate, Upper Egypt, using remote sensing and aeromagnetic data

Provisionally accepted
Hussein T. El-Badrawy Hussein T. El-Badrawy 1Abbas M. Abbas Abbas M. Abbas 2Usama Massoud Usama Massoud 2Tamer Abu-Alam Tamer Abu-Alam 3*Hamed A. Alrefaee Hamed A. Alrefaee 1Saif Abo Khashaba Saif Abo Khashaba 1Mostafa Nagy Mostafa Nagy 1*
  • 1 Department of Geology, Faculty of Science, Kafrelsheikh University, Kafr Elsheikh, Egypt
  • 2 National Research Institute of Astronomy and Geophysics, Helwan, Cairo, Egypt
  • 3 Department of Arctic and Marine Biology, Faculty of Biosciences, Fisheries and Economics, UiT The Arctic University of Norway, Tromsø, Troms, Norway

The final, formatted version of the article will be published soon.

    Groundwater demand has been considerably heightened due to rapid urban growth, specifically in arid areas that rely primarily on groundwater. This study aims to utilize remote sensing and aeromagnetic data, combined with the Analytic Hierarchy Process (AHP) based GIS, to evaluate potential groundwater zones in the Sohag area, Egypt. Nine thematic layers, including soil moisture, rainfall, lithology, normalized difference vegetation index (NDVI), drainage density, lineament density, slope, and land use/land cover, were developed using various remote sensing datasets. Besides the remote sensing-derived thematic layers, a geophysics-derived thematic layer represented by the RTP aeromagnetic map was included. The groundwater potentiality map was consistent with production wells in the area, and sites for drilling new wells were predicted, especially in the Nile Valley around the Tahta, El-Hamimia, and west Sohag cities. The most promising sites are clustered along the Nile Valley, and the study area's northwestern and Note: Revised manuscript with tracked changes and a clean copy of the manuscript in the same file. northeastern parts. The aeromagnetic data were analyzed and interpreted to outline the subsurface structure affecting groundwater storage and flow. Also, the aeromagnetic data analysis helps estimate the basement depth that constitutes the Nubian Aquifer's base and identifies regions with considerable thick sedimentary deposits and significant water reserves. The results indicate that the predominant magnetic structural trends are NW-SE, NE-SW, N-S, and E-W, which contribute to the formation of a series of subsurface horsts (H) and grabens (G). Three main basins (A, B, and C) were identified as the most profound areas. These basins represent the most promising areas for groundwater accumulation, making them attractive for future hydrogeological exploration. This integrated approach strongly offers a powerful and effective tool to assist in developing an appropriate plan to manage groundwater in arid regions. technique that integrates subjective judgments and multiple evaluation factors to complement the decision-making process. By following this systematic AHP-based approach, researchers and decision-makers can effectively combine quantitative data and subjective expert opinions to delineate groundwater potential areas, supporting more informed groundwater management and exploration strategies (

    Keywords: remote sensing, Radar data, Aeromagnetic, Groundwater potentiality, Sohag

    Received: 27 Jun 2024; Accepted: 29 Aug 2024.

    Copyright: © 2024 El-Badrawy, Abbas, Massoud, Abu-Alam, Alrefaee, Abo Khashaba and Nagy. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

    * Correspondence:
    Tamer Abu-Alam, Department of Arctic and Marine Biology, Faculty of Biosciences, Fisheries and Economics, UiT The Arctic University of Norway, Tromsø, 9019, Troms, Norway
    Mostafa Nagy, Department of Geology, Faculty of Science, Kafrelsheikh University, Kafr Elsheikh, Egypt

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