Lineaments Detection and Groundwater Exploration Using GIS and Geo-electric Data at Wadi El-Asyuti Area, Eastern Desert, Egypt. | ||||
| Al-Azhar Bulletin of Science | ||||
| Article 12, Volume 32, Issue 2-D, December 2021, Page 49-59 PDF (1.64 MB) | ||||
| Document Type: Review Article | ||||
| DOI: 10.21608/absb.2021.84781.1125 | ||||
 View on SCiNiTO | ||||
| Authors | ||||
Ashraf M. Abdo  1; Hassan S. Sabet1; Mohamed E. Mebed2
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| 1Geology Department, Faculty of Science, Al-Azhar University, Cairo, Egypt. | ||||
| 2Geophysics Management, Egyptian Mineral Resources Authority, Egypt. | ||||
| Abstract | ||||
| Geo-electric and GIS data toWadi El-Asyutiarea, central Eastern Desert, Egypt have been used for identify the different lineaments and possibilities of the occurrence of the groundwater.Shaded relief maps were developed from the digital elevation model (DEM) which used for identifying the lineaments. Geomatica software extracted the lineaments at the final maps with NW-SE direction.Meanwhile the geologic fault trends derived from geologic map take NW-SE, WNW-ESE, N-S and ENE-WSW directions. Twenty two electric resistivity soundings were conducted in the study area and three cross sections. Drilled well is near from VES-22. Geo-electric and drilling results reflected three layers. The first one consists of Wadi deposit, friable sand, fine sand, clay and limestone. The second layer composed of clay intercalation with limestone and silt and the third layer consists of clay intercalation with sand and silt and represented the aquifer layer. | ||||
| Keywords | ||||
| Wadi El-Asyuti area; Digital elevation model (DEM); Electric resistivity soundings; Groundwater | ||||
| References | ||||
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[1] Bakheit, A A. Geological and geophysical studies on the areas around Wadi El-Assiuti, Eastern Desert, Egypt. Ph.D. Thesis, Geol. Dept., Assiut Univ.1989; 203. p.
[2] Ashmawy, M H and Nassim, A S. Hydrogeologic impact and assessement of morphometric aspects of wadi el Asyuity basin, Eastern desert, Egypt.Tanta University. Egyptian journal of remote sensing and space science.1998; vol.1, no.1: pp.207-232.
[3] Mohamaden, M I.Geoelectrical Survey for Groundwater Exploration at the Asyuit Governorate, Nile Valley, Egypt. Marine Scienes.2009; 20 (1).
[4] Abotalib, A Z and Mohamed, R S. Surface evidences supporting a probable new concept for the river systems evolution in Egypt. A remote sensing overview. 2013; 69(5): pp.1621-1635.
[5] El Tahlawi, M R, Abo-El Kassem, M, Baghdadi, G Y and Saleem, H A. Assessment of groundwater Vulnerability a case study. International Journal of Advanced Remote Sensing and GIS.2016; pp-1561.
[6] Refaat, m. Integrated Interpretaion of land Geophysical surveys and Remote Sensing data for groundwater horizons detection at new assiut city- el safa city, western desert Egypt. M.Sc. Thesis, Geol. Dept., al-azhar Univ.2018.
[7] Conoco. Geological Map of Egypt, Scale 1: 500,000, -NG 36NW- Asyut, Egypt. The Egyptian General Petroleum Corporation, Cairo (EGPC), Egypt.1987.
[8] Abdallah, M S. the Najd Fault System. King Fahd University of Petroleum & Minerals. 2016; https://www.researchgate.net/ation/3public13881827_The_Najd_Fault_System.
[9] http://earthexplorer.usgs.gov.
USGS: Science for a changing world. U.S. Department of the Interior U.S. Geological Survey- Page Contact Information:custserv@usgs.gov.
[10] Zohdy, A A R and Bisdorf, R J. Programs for the automatic processing and interpretation of Schlumberger sounding curves in Quick Basic; U.S. Geological Survey Open File Report .1989; 89-137-2, 64 p.
[11] Velpen, B P A. Resist program, M.Sc. Research project, ITC, Holland.1988;v.1.0.
[12] Sadek, H S, Soliman, S A and Abdulhadi, H M. A correlation between the different models of resistivity sounding data to discover new fresh water fields in El Sadat City, Western Desert of Egypt. Proc. of the 7PUthUP International Mathematical Geophysics Seminar, Free University of Berlin. 1987; 329-346. | ||||
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