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Volume 8 Issue 2
Jun.  2020
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Article Navigation >  Journal of Groundwater Science and Engineering  > 2020  >  8(2): 172-179
Fatima Zahra FAQIHI, Anasse BENSLIMANE, Abderrahim LAHRACH, et al. 2020: Recognition of the hydrogeological potential using electrical sounding in the KhemissetTiflet region, Morocco. Journal of Groundwater Science and Engineering, 8(2): 172-179. doi: 10.19637/j.cnki.2305-7068.2020.02.008
Citation: Fatima Zahra FAQIHI, Anasse BENSLIMANE, Abderrahim LAHRACH, et al. 2020: Recognition of the hydrogeological potential using electrical sounding in the KhemissetTiflet region, Morocco. Journal of Groundwater Science and Engineering, 8(2): 172-179. doi: 10.19637/j.cnki.2305-7068.2020.02.008
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Recognition of the hydrogeological potential using electrical sounding in the KhemissetTiflet region, Morocco

doi: 10.19637/j.cnki.2305-7068.2020.02.008

  • 1Laboratory Géodynamics and Natural Ressources, Faculty of Sciences Dhar El Mahraz, University Sidi Mohamed Ben Abdellah, PB 1796 Fez-Atlas30003, Morocco.2Laboratory of Georessourcesand Environment, Faculty of Sciences and Technique, University Sidi Mohamed Ben Abdellah, FES PB 2202-Route d’Imouzzer, FES-Morocco.3Laboratory of Geosciences of Natural Resources, Faculty of Sciences, University Ibn Tofail, PB 133, Kenitra Morocco.

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Fatima Zahra FAQIHI

    Abstract
  • The low recharge of reservoirs and the increasing demand for water limit the potential of mobilized resources, especially in arid to semi-arid areas like Morocco. Integrated management is essential to safeguard this resource. In respect with this perspective, this work provides the analysis of hydrogeological potential of Khemisset-Tiflet region, which falls within the action area of the Sebou Hydraulic Basin Agency. The basis of our studies was as follows: (1) The interpretation of the existing geoelectric data; (2) application of geophysical methods for non-destructive reconnaissance and their integration into a Geographic Information System (GIS). The analysis demonstrates that: The map of the isohypses and the geoelectric cross-section of the substratum of the superficial roof aquifer show clearly a plunge associated with development of the Paleozoic roof in the South and the direction of flow of the surface water is from south to north, from the upper zone to the north of the El Kansera dam. These conclusions constitute very useful contribution for any resource management projects in this area.
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