Delineation of saltwater intrusion into the freshwater aquifer of Lekki Peninsula, Lagos, Nigeria

• Published in: Environmental earth sciences Vol. 56; no. 5; pp. 927 - 933
• Main Authors: Adepelumi, A. A, Ako, B. D, Ajayi, T. R, Afolabi, O, Omotoso, E. J
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Berlin/Heidelberg : Springer-Verlag 2009; Springer Berlin Heidelberg; Springer; Springer Nature B.V
• Subjects: Aquifers; Coastal zone; Earth and Environmental Science; Earth Sciences; Earth, ocean, space; Electrical resistivity; Electrodes; Exact sciences and technology; Geochemistry; Geology; Geophysics: general, magnetic, electric and thermic methods and properties; Groundwater; Hydrogeology; Hydrology. Hydrogeology; Internal geophysics; Lithology; Mineralogy; Original Article; Saline water; Saline water intrusion; Salinity; Saturated soils; Silicates; Studies; Water geochemistry; Water quality; Nigeria; West Africa; Africa; Lagos Nigeria; ANE, Portugal, Faro, Lagos; Coastal; Saline water; Nigeria; Aquifer; Resistivity; rock matrix; mixing; lithology; ground water; saturation; brines; coastal zone; transition zones; aquifers; hydrochemistry; soils; electrical resistivity; salinity; electrodes; salt-water intrusion; electrical sounding; subsurface; infiltration; coastal environment; sand; depth; water quality; fresh water
• DOI: 10.1007/s00254-008-1194-3
• ISSN: 0943-0105; 1866-6280

Recently, the deterioration of water quality in the coastal zones of Lekki Peninsula area of Lagos due to saltwater infiltration into the freshwater aquifer has become a major concern. With the aim of providing valuable information on the hydrogeologic system of the aquifers, the subsurface lithology and delineating the groundwater salinity, vertical electrical resistivity (VES) sounding survey was carried out utilizing surface Schlumberger electrode arrays, and electrode spacing varying between 1 and 150 m. The DC resistivity surveys revealed significant variations in subsurface resistivity. Also, the VES resistivity curves showed a dominant trend of decreasing resistivity with depth (thus increasing salinity). In general, the presence of four distinct resistivity zones were delineated viz.: the unconsolidated dry sand (A) having resistivity values ranging between 125 and 1,028 Ωm represent the first layer; the fresh water-saturated soil (zone B) having resistivity values which correspond to 32-256 Ωm is the second layer; the third layer (zone C) is interpreted as the mixing (transition) zone of fresh with brackish groundwater. The resistivity of this layer ranges from 4 to 32 Ωm; while layer four (zone D) is characterized with resistivities values generally below 4 Ωm reflecting an aquifer possibly containing brine. The rock matrix, salinity and water saturation are the major factors controlling the resistivity of the formation. Moreover, this investigation shows that saline water intrusion into the aquifers can be accurately mapped using surface DC resistivity method.