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2019 | 23 |

Tytuł artykułu

Geophysical survey of basement complex terrain using electrical resistivity method for groundwater potential

Treść / Zawartość

Warianty tytułu

Języki publikacji

EN

Abstrakty

EN
A geophysical survey of basement complex using electrical resistivity method was carried out so as to provide geological and geophysical information on the different subsurface features. The soughtfor parameters include thickness, depth, basement for groundwater potential and aquifer protective capacity. The acquired data were process using Win-Resist software and surfer 8, and the result was then analyzed and interpreted. Accordingly, 3-4 geoelectrical layers within the subsurface delineate the area: top soil, lateritic layer, weathered/fractured layer and fresh rock. Resistivity values of the top soil range between 55.5 mΩ to 749.7 mΩ, with average thickness of 0.4 m to 3.6 m, while the lateritic layer ranges between 153.3 mΩ to 862.0 mΩ, with average thickness of 4.5 m to 20.7 m, the weathered/fractured layer in turn ranges between 15.6 mΩ to 698.9 mΩ, with average thickness of 7.7 m to 55.2 m, and the fresh rock ranges between 13.4 mΩ to 5102 mΩ, with infinite homogeneous half space. Over all, the longitudinal conductance of the overburden units range from 0.147 mhos to 0.957 mhos and the overburden is thick enough for groundwater exploration activities. The results provide reasonably information that the aquifer units are weathered/fractured layers with a significant groundwater potential that is free of contamination.

Słowa kluczowe

Wydawca

-

Rocznik

Tom

23

Opis fizyczny

p.154-165,fig.,ref.

Twórcy

autor
  • Department of Physics, University of Abuja, Abuja, Nigeria
  • School of Physics, Universiti Sains Malaysia, Penang, Malaysia
autor
  • Department of Physics, University of Abuja, Abuja, Nigeria
  • School of Physics, Universiti Sains Malaysia, Penang, Malaysia
autor
  • Department of Physics, University of Abuja, Abuja, Nigeria

Bibliografia

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  • [4] Mohamaden MII, Delineating groundwater aquifer and subsurface structures by using geoelectrical data: Case study (Dakhla Oasis, Egypt). NRIAG Journal of Astronomy and Geophysics 5 (2016) 247–253. doi.org/10.1016/j.nrjag.2016.05.001
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  • [9] Maiti S, Erram VC, Gupta G, Tiwari RK, ANN based inversion of DC resistivity data for groundwater exploration in hard rock terrain of western Maharashtra (India). Journal of Hydrology 464–465 (2012) 294–308.
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  • [18] Nwachukwu MA, Nwosu I, Uzoije PA, Nwoko CA, 1D resistivity inversion technique in the mapping of igneous intrusives; A step to sustainable quarry development. Journal of Sustainable Mining 16(4) (2017) 127-138. doi.org/10.1016/j.jsm.2017.11.001
  • [19] Adeeko TO, Samson DO, Application of Electrical Resistivity in Mapping Subsurface Characteristics. Asian Journal of Environment & Ecology 6(2) (2018) 1-12. doi: 10.9734/AJEE/2018/40096
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Typ dokumentu

Bibliografia

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Identyfikator YADDA

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