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Pure and Applied Geophysics

, Volume 175, Issue 6, pp 2251–2267 | Cite as

Geophysical and Hydrogeological Evaluation of Pliocene Aquifer in East Esna, Egypt

  • Alhussein Adham BasheerEmail author
  • Sayed Mosaad
Article
  • 112 Downloads

Abstract

The current study of East Esna area was selected due to its prosperous conditions. In this area, the reclamation of agricultural land is increasing and the population is growing, which necessitate an equivalent development of groundwater. The main aim of the study was to estimate geometrical and qualitative characteristics of the study aquifer. This will help to have a systematic view of the hydrogeological setting in the area of investigation, categorize and evaluate the influential factors of existence, quality, and protection of the groundwater. The geometrical characteristics of the local aquifer were revealed by using 45 VES and TEM soundings. The study area has two main aquifers. Both hosted in sandstone of Issawia formation. The brackish groundwater lies above the fresh groundwater, which is shielded by Esna shale at the bottom. The source of feeding to these aquifers is direct leakage of runoff and rain on the east side with sporadic leaks from the waters of the River Nile on the west side. The analyzed groundwater samples are geochemically homogenous, indicating that their genesis is rain water. They also belong to Na–Ca–SO4–Cl type. The groundwater in the study area is assessed for drinking, household, livestock, and agricultural purposes. The current study recommends some advises for groundwater development in the study area.

Keywords

Geophysical investigation geochemical evaluation hydrological aspects East Esna aquifer potentiality 

References

  1. Abdel, M. M., Faid, A., Ismail, E., & Schöniger, M. (2014). Groundwater management in the Esna City, Upper Egypt: An application of remote sensing and numerical modeling. Natural Resources, 2014(5), 732–745.  https://doi.org/10.4236/nr.2014.512063.CrossRefGoogle Scholar
  2. Ahmed, A., May A. (2013). Fluoride in quaternary groundwater aquifer, Nile Valley, Luxor, Egypt. Arab Journal of Geoscience. 7, 3069–3083.  https://doi.org/10.1007/s12517-013-0962-x.
  3. Attia, F. A. R., Allam, M. N., & Amer, M. A. (1986). A hydrologic budget analysis for the Nile Valley in Egypt. Groundwater, 24, 453–459.CrossRefGoogle Scholar
  4. Brikowski, T. H., & Faid, A. M. (2006). Pathline-calibrated groundwater flow models of Nile Valley Aquifers, Esna, Upper Egypt. Journal of Hydrology, 324(1–4), 195–209.  https://doi.org/10.1016/j.jhydrol.2005.10.011.CrossRefGoogle Scholar
  5. Conoco (1987) Geologic Map of Egypt. Egyptian General Authority for Petroleum (UNESCO Joint Map Project), 20 Sheets, Scale 1:500 000, Cairo.Google Scholar
  6. El Abde, E. A., Shaba, A. R., & El Sheikh, A. E. (2011). Hydrogeological evaluation of west Deirout-Assuit area, Egypt. Egyptian Journal of Geology, 55(201), 211–226.Google Scholar
  7. Faid, A. (2003). Integrate of Geoelectrical data to Identify Aquifers and Paleo-Channel in Esan Area Upper Egypt. Science Journal Faculty of Science, XVII, 89–118.Google Scholar
  8. Faid, A.M., & Brikowski, T.H. (1994). Determining groundwater development potential of Nile Valley Aquifers, Esna, Egypt. Groundwater, 24. M.Sc. Thesis, University of Ain Shams, Cairo.Google Scholar
  9. Issawi, B., Hassan, M., Attia, S. (1978). Geology of Abu Tartur Plateau, Western Desert, Egypt. Annals of the Geological Survey of Egypt, 8, 91e127.Google Scholar
  10. Elmagd, K.A., Ali-Bik, M.W., Abayazeed, S.D., (2014). Geology and geochemistry of Kurkur bentonites, southern Egypt: provenance, depositional environment, and compositional implication of Paleocene–Eocene thermal maximum, Arabian Journal of Geosciences, 7(3), 899–916.Google Scholar
  11. Mckee, J. E., & Wolf, H. W. (1963). Water quality criteria. California: California State Water Quality Board Publ. 3-A.Google Scholar
  12. Mohammed, A., Krishnamurthy, R. V., Kehew, A. E., Crossey, L. J., & Karlstrom, K. K. (2016). Factors affecting the stable isotopes ratios in groundwater impacted by intense agricultural practices: A case study from the Nile Valley of Egypt. Science of the Total Environment, 573(2016), 707–715.CrossRefGoogle Scholar
  13. Morgan, P. (1990). Egypt in the framework of global tectonics. In: Said R., (Ed.), The Geology of Egypt, Chap. 7 (pp. 91–112). Rotterdam: A.A. Balkema Publishers.Google Scholar
  14. Piper, AM. (1944). A graphic procedure in the geochemical interpretation of water analyses. Transactions, American Geophysical Union. 25(6), 914–928.  https://doi.org/10.1029/TR025i006p00914.
  15. RIGW (1994). Hydrogeological Map for West ESNA Scale 1:100000, Free Atlas project for Hydrogeological Maps of the South western Desert Egypt. Academy of Scientific Research and Technology (ASRT) in association with [Capacity Building of the Egyptian Survey and Mining Authority and the National Authority for Remote Sensing and Space Sciences] in cooperation with UNDP and UNESCO.Google Scholar
  16. Sadek, M. A., & Abd El–Samie, S. G. (2001). Pollution vulnerability of the quaternary aquifer near Cairo, Egypt, as indicated by isotopes and hydrochemistry. Hydrogeology Journal, 9, 273–281.CrossRefGoogle Scholar
  17. Said R. (1981). The Geological Evolution of the River Nile. viii + 151 pp., 73 figs. Berlin: Springer. Price DM 148.00; U.S. $68.90. ISBN 3 540 90484 0.Google Scholar
  18. Said R. (ed.) (1990). The Geology of Egypt. Rotterdam, Brookfield: A. A. Balkema, x + 734 pp. Price £51.00 (hard covers). ISBN 90 6191 856 1.Google Scholar
  19. Schoeller, H. (1962). Les eaux souterraines [Groundwater]. Paris: Massio et Cie.Google Scholar
  20. SIROTEM MK3 (2003). Electromagnetic instrument, Australian Society of Exploration Geophysics, PO Box 576, Crows Nest NSW 1585. https://www.aseg.org.au/sirotem, User manual. http://ngpampappnmepgilojfohadhhmbhlaek/captured.html?back=1.
  21. Soliman, S. (1996). Environmental hydrologic impacts of the new esna barrage and the land reclamation activities. Cooperated with Institute Of Envirnomental Studies & Researches, Department Of Engineering Sciences. Thesis (M.D), Ain Shams University, Egypt.Google Scholar
  22. Syscal/R2. High-power system of DC electrical surveys, IRIS Company for Instruments, 2014, 1 avenue Buffon, 45100 Orleans, France. http://www.iris-instruments.com/syscal-r2.html.
  23. TEMIXL XL program V4. (1996). Temix v. 4 user’s manual, Interpex, p 468.Google Scholar
  24. Toth, J. (1999). Groundwater as a geologic agent: an overview of the causes, processes, and manifestations. Hydrogeology Journal, 7(1), 1–14.CrossRefGoogle Scholar
  25. U.S. Salinity Laboratory Staff. (1954). Diagonsis and improvement saline and alkali soil: Agric, handbook, 60 (pp. 1–60). Washington DC: U.S. Salinity Laboratory Staff.Google Scholar
  26. World Health Organization (WHO) (2011). The guidelines for drinking-water quality, a summary of the progress made towards achieving the health-related Millennium Development Goals (MDGs) and associated targets, 4th edn, p 564. ISBN 978 92 4 154815 1. http://www.who.int/whosis/whostat/2011/en/
  27. Zond 1D program (2017). One-dimensional resistivity and induced polarization vertical electrosounding data interpretation, Russia 195009, Saint-Petersburg, Bobruyskaya. http://zond-geo.ru/english/zond-software/ert-and-ves/zondip1d/.

Copyright information

© Springer International Publishing AG, part of Springer Nature 2018

Authors and Affiliations

  1. 1.Geology Department, Faculty of ScienceHelwan UniversityCairoEgypt

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