The best Side of Ita-Eku state Ekiti
The best Side of Ita-Eku state Ekiti
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Electrical resistivity prospecting strategy was Utilized in analyzing the groundwater likely of Ita-Eku, southeastern A part of Ado-Ekiti, Ekiti state, Nigeria using the vertical electrical sounding method. A complete of 7 electrical soundings were performed using the Schlumberger electrode array. The data obtained ended up interpreted qualitatively and quantitatively and ended up presented as tables, charts and area. The interpreted models discovered three to four geo-electric powered levels namely; topsoil, clay/lateritic soil, weathered/fractured layer and fresh new basement. The topsoil which is fairly thin has thickness ranging among 0.eight and a pair of.5m whilst the resistivity values range from 26 to 171 Ω-m. The next layer has thickness starting from 2.
Nobody may give exact dates to those activities a result of the not enough published resources, but people have lived in Ekiti for hundreds of years. It's on report that Ekiti Obas experienced a prosperous reign in the 13th century. An instance was the reign of Ewi Ata of Ado-Ekiti during the 1400s.
southwestern Nigeria, It's a city surrounded by hills and inselbergs of various styles in ridges, a rugged
or fluid passage in basement ecosystem this end result into fracture zone .This zone have reduced resistivity price
The Basement Advanced of Africa is a heterogeneous Ita-Eku state Ekiti combination of crystalline rocks, predominantly of the granitic or gneissose character. Groundwater happens within just these crystalline rocks in fissures or from the superficial weathered zones.
groundwater probable throughout the weathered/ fractured zone. Based on the localized mother nature of aquifer found in
The study with the groundwater opportunity and aquifer protecting potential of overburden units in Ado-Ekiti, Ekiti State, southwestern Nigeria have been carried out. The region is underlain by the Precambrian basement elaborate of southwestern Nigeria with local geology predominantly granite-gneiss and migmatite. 51 Schlumberger vertical electrical soundings (VES) were being lined. The interpretation unveiled three distinctive geoelectric layers overlying the resistive basement, the topsoil, the weathered layer along with the partly weathered/fractured basement. The depth to the very best of basement (overburden thickness) assorted from one.
meter. The resistivity meter is a high quality earth resistance meter effective at accurate
resistivity sounding these ended up computed with the VES result, other parameters regarded as are longitudinal
second electrical resistivity tommorgraphy for environmental, engineering and hydrogeological software in Igarra, Nigeria
The water supply needs to be verified and created before the pricey infra construction—the manufacturing facility or distribution community—is developed.
Ado- Ekiti can be a town surrounded with hills and ridges a basement complicated setting; it lies about the
greater elevation to reduced elevation parts. Drinking water converges into reduced depth location with blue colour. The
The examine region handles about 1875km2 close to Gusau in northwestern Nigeria. The basement rocks of your district comprise migmatites, gneisses, metasediments and granitic Intrusives. Out there borehole ilothological logs reveal that these happen to be appreciably weathered to distinct depths. These weathered portions which overly the new bedrocks constitute the aquifer. Hydrogeological sections interpreted from VES curves for that regolith, clearly show that the vast majority of regions have four geoelectric layers.