Abstract
The current study would use geophysical investigations and geo-informatics to assess the groundwater aquifer at Wadi Dawqah–Al Baha. The morphometric analysis of the drainage basins gives a complete picture of the best catchment areas for surface water, which consider the main feeder for the groundwater aquifer. For the area drainage basin, a digital elevation model, slope, aspect, and drainage pattern maps were developed. The drainage pattern of the study area appears to be dendritic, with five major tributaries converging at the study area. Various metrics for calculating drainage basin morphometry, such as stream number, flow order, flow length ratio, bifurcation ratio, basin length, basin area, relief ratio, streaming density, flow rate, shape factor, and circulation ratio have been studied using conventional mathematical formulas. Eighteen vertical electrical soundings (VES) were conducted using a Shlumberger array with a maximum AB/2 of 200 m. While the time domain electromagnetic (TDEM) survey was conducted at eight different locations along the Wadi using a coincident loop configuration in which signals were transmitted and received using the same loop. The effects of the interpreted VES and TDEM soundings are used to create a variety of cross-sections and maps of resistivity, thickness, and depth of the aquifer layer. These maps display a smooth distribution of aquifer resistivity values ranging from 30 to 190 Ω m. The average thickness of the water saturated Wadi deposits (aquifer) layer ranges from 16 to 50 m. The aquifer depth shows moderate values ranging from 14 to 26 m. On the other hand, the presence of four geoelectric layers is detected in the built resistivity cross-sections along some profiles. The resistivity values and average thickness of each layer were identified and their corresponding interpreted geological cross-sections were constructed.













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Abd El-Gawad AMS, Ammar AI (2004) The contribution of geoelectrical investigations in delineating the shallow aquifer in Wadi El Natrun area, Western Desert. Egypt EGS J 2(1):37–50
Araffa SA, Soliman SA, El Khafif A, Younis A, Shazley TF (2019) Environmental investigation using geophysical data at East Sadat City. Egypt Egypt J Pet 28:117–125
Clarke JI (1996) Morphometry from maps. Essays in geomorphology. Elsevier publication. Co., New York, pp 235–274
Emenike EA (2001) Geophysical exploration for ground water in a sedimentary environment. Global J Pure Appl Sci 7(1):97–102
Fitterman DV, Stewart MT (1986) Transient electromagnetic sounding for groundwater. Geophysics 51(4):995–1005
Gabr S, Morsy E, El Bastawesy M, Abeebullah TM, Shaaban F (2017) Exploration of potential groundwater resources at Thuwal area, north of Jeddah, Saudi Arabia, using remote sensing data analysis and geophysical survey. Arab J Geosci. https://doi.org/10.1007/s12517-017-3295-3
Greenwood WR (1975) Geology of the Jabal Shada quadrangle, sheet 19/41 A, Kingdom of Saudi Arabia: Saudi Arabian Directorate General of Mineral Resources Geologic Map GM-20, 10 p., scale 1:100,000.
Horton RE (1945) Erosional development of streams and their drainage basins; hydrophysical approach to quantitative mor- phology. Bull Geol Soc Am 56:275–370
IX1D (2016) Interpex software high quality affordable software for the processing, interpretation and display of geophysical data. http://www.interpex.com/ix1dv3/ix1dv3.htm. Accessed 16 June 2021
Khalil MA, Abbas AM, Santos F, Massoud U, Salah H (2013) Application of VES and TDEM techniques to investigate sea water intrusion in Sidi Abdel Rahman area, northwestern coast of Egypt. Arab J Geosci 6:3093–3101
Massoud U, El Qady G, Metwaly M, Santos F (2009) Delineation of shallow subsurface structure by azimuthal resistivity sounding and joint inversion of VES–TEM data: case study near Lake Qaroun, El Fayoum. Egypt Pure Appl Geophys 166(2009):701–719
Massoud U, Santos F, Khalil M, Taha A, Ali A (2010) Estimation of aquifer hydraulic parameters from surface geophysical measurements: a case study of the Upper Cretaceous aquifer, central Sinai, Egypt. Hydrol J 18(3):699–710. https://doi.org/10.1007/s10040-009-0551-y
Merritts D, Vincent KR (1989) Geomorphic response of coastal streams to low, intermediate, and high rates of uplift, Mendocino junction region, northern California. Geol Soc Am Bull 101:1373–1388
Metwaly M, Elawadi E, Moustafa SSR, Al-Arifi N (2014) Combined inversion of electrical resistivity and transient electromagnetic soundings for mapping groundwater contamination plumes in Al Quwy’yia Area. Saudi Arabia JEEG 19(1):45–52
Muller JE (1968) An introduction to the hydraulic and topographic sinuosity indexes. Ann Assoc Am Geogr 58:371–385
Nabighian MN, Macanae JC (1991) Time-domain electromagnetic prospecting methods. In: Nabighian MN (ed) Electromagnetic methods in applied geophysics, vol 2. Society of Exploration Geophysics, Tulsa, pp 427–514
Re V, Zuppi GM (2011) Influence of precipitation and deep saline groundwater on the hydrological systems of Mediterranean coastal plains: a general overview. Hydrol Sci J 56(6):966–980. https://doi.org/10.1080/02626667.2011.597355
Rubin Y, Hubbard SS (2005) Hydro geophysics. Springer, The Netherlands, p 583
Strahler AN (1952) Hypsometric analysis of erosional topography. GSA Bulletin 63(11):1117–1142
Strahler AN (1964) Quantitative geomorphology of drainage basins and channelnetworks. In: Chow VT (ed) Handbook of applied hydrology. McGraw-Hill, New York, pp 439–476
Vereecken H, Yaramanci U, Kemna A (2002) Non-invasive methods in hydrology special issue. J Hydrol 267:125–299
Vereecken H, Hubbard S, Binley A, Ferre T (2004) Hydrogeophysics. Introd Guest Ed Vadose Zone J 3:1060–1062
Younis A, Soliman M, Moussa S, Massoud M, Abd El Nabi S, Attia M (2016) Integrated geophysical application to investigate groundwater potentiality of the shallow Nubian aquifer at northern Kharga, Western Desert. Egypt NRIAG J Astron Geophys 5(2016):186–197
Zohdy AR (1989) A new method for the automatic interpretation of Schulmberger and Wenner sounding curves. Geophysics 54:245–253
Zohdy AAR, Martin RJ (1993) A study of seawater intrusion using direct current sounding in the southern part of the Oxward Plain, California. U.S. Geological Survey
Zond (2016) Program for one-dimensional data interpretation of transient electromagnetic method using arbitrary source-receiver configuration. (loop/line/ dipole) version 5.2.
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The authors would like to thank the Deanship of Scientific Research at Umm Al-Qura University for supporting this work by Grant Code: (22UQU4361180DSR01).
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Shaaban, F., Taha, A.I., Othman, A. et al. An integrated geoinformatics and hydrogeophysical approach to assess and characterize the alluvial aquifer of Wadi Dawqah, southwestern Saudi Arabia. Environ Earth Sci 81, 259 (2022). https://doi.org/10.1007/s12665-022-10367-z
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DOI: https://doi.org/10.1007/s12665-022-10367-z


