GEOTECHNICAL INVESTIGATION OF THE PROPOSED IFE DAM SITE AT KAJOLA VILLAGE, ILE-IFE, SOUTHWESTERN NIGERIA

O. Ajayi, K. Adekoya, O. P. Egwuatu, C. I. Konwea
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Abstract

Geological and geophysical investigations were conducted to assess the competence and structural integrity of the foundation site of the proposed Ife-dam at Kajola Village, Ile-Ife, Southwestern Nigeria. Geological investigation along the two (2) proposed dam axes revealed that the overburden material is loose to dense with angular shearing resistance (ɸ) of 27o to 41o. The soils are predominantly elastic silts; cohesive with considerable strength and stability. Geophysical investigation involving the Schlumberger Vertical Electrical Sounding delineated four (4) lithologies namely: topsoil with resistivity of 69 – 558 Ωm and thickness between 1.5 and 4.0 m; weathered sandy layer with resistivity from 123 – 586 Ωm and thickness between 6.5 and 20.4 m; partially weathered/ fractured basement with resistivity from 60 – 220 Ωm and thickness between 6.5 and 14.0 m; and the fresh basement rock with resistivity from 1337 – 10683 Ωm. There are indications of fractures at a depth of 32 m beneath Axis B extending to Axis A at a depth of 35 m. The subsurface materials are suitable to host a dam. Axis B is more appropriate for the dam axis, although the fracture zone should be factored into the design of the dam to prevent water seepage.
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尼日利亚西南部伊莱伊夫卡约拉村拟建的伊莱伊夫大坝遗址的岩土工程调查
在尼日利亚西南部伊莱-伊莱卡约拉村进行了地质和地球物理调查,以评估拟议的伊莱-伊莱坝地基的能力和结构完整性。沿两(2)条坝体轴线进行的地质调查表明,坝体覆盖层松散至致密,角抗剪系数为27 ~ 41。土壤主要是弹性粉砂;具有相当的强度和稳定性。包括斯伦贝谢垂直电测深在内的地球物理调查圈定了四(4)种岩性,即:表土电阻率为69 - 558 Ωm,厚度在1.5 - 4.0 m之间;风化砂层,电阻率123 ~ 586 Ωm,厚度6.5 ~ 20.4 m;部分风化/裂缝基底,电阻率60 ~ 220 Ωm,厚度6.5 ~ 14.0 m;新鲜基岩电阻率1337 ~ 10683 Ωm。有迹象表明,B轴下方32m处存在裂缝,裂缝延伸至35m处的a轴。地下材料适合建坝。B轴为坝轴线更合适,但坝体设计中应考虑断裂带,防止渗水。
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