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首页> 外文期刊>Research Journal of Applied Sciences: RJAS >Geophysical Investigation of Damsite in a Sedimentary Terrain: A Case Study
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Geophysical Investigation of Damsite in a Sedimentary Terrain: A Case Study

机译:沉积地形中坝体的地球物理研究:一个案例研究

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Geophysical investigation was carried out at a site in Okada town near Benin City, southwsetern Nigeria, in order to evaluate the suitability of the area for a damsite. The survey was conducted along the proposed dam axis (about 850 m long) and its vicinity by using Vertical Electrical Sounding to unravel the subsurface profile, which in turn determines if there would be any subsurface lithological variation (s) that might lead to structural failure in the dam foundation. To achieve the above objectives, six sounding stations were located and fully occupied along the dam axis while 2 VES were conducted close to the dam axis. The data obtained were subjected to 1-D inversion algorithm to determine the layer parameters. The results show that the subsurface is remarkably inhomogeneous in geological composition. The geoelectric section revealed four to 5 lithologic units defined by the topsoil, lateritic hard pan, dry sandy formation and various combinations of sandy clay, clayey sand and sand as constituting the subsurface of the proposed damsite. Resistivity values range from 1422-6895, 1201-10525, 1820-3606 and 105-9270 m in the topsoil, lateritic hard pan, dry sand formation and the clayey sand/sandy clay/sand layer(s), respectively. Layer thicknesses vary from 0.5-2.0 m in the topsoil, 1.4-8.2 and 6.5-31.2 m in the lateritic hard pan and dry sandy formation, respectively. Based on these results, it is concluded that the subsurface material in the study area is highly competent to withstand the load of the proposed dam. However, resistivity values <200 m at depths below about 31.7 m indicate high porosity, high clayey sand content and high degree of saturation, which are indicators of soil conditions requiring serious consideration in the design of the dam.
机译:在尼日利亚西南部贝宁市附近的冈田镇的一个地点进行了地球物理调查,以评估该区域是否适合坝址。该勘测是沿着拟建的大坝轴线(约850 m长)及其附近地区进行的,方法是使用垂直电测深仪揭示地下剖面,这反过来确定是否存在可能导致结构破坏的地下岩性变化。在大坝基础上。为了实现上述目标,沿着坝轴线设置了六个测深站并完全占据,而在坝轴线附近进行了2个VES。对获得的数据进行一维反演算法以确定层参数。结果表明,地下的地质组成明显不均匀。地电部分揭示了由表层土壤,红土硬盘,干砂质地层和砂质粘土,黏性砂和砂的各种组合定义的4至5个岩性单元,构成了拟建坝体的地下。在表层土壤,红土硬盘,干砂地层和黏土砂/砂质粘土/沙层中,电阻率值分别为1422-6895、1201-10525、1820-3606和105-9270 m。表土的层厚分别为0.5-2.0 m,红土硬盘层和干砂层的层厚分别为1.4-8.2和6.5-31.2 m。基于这些结果,可以得出结论,研究区域的地下材料非常有能力承受拟建大坝的负荷。然而,在低于约31.7 m的深度处,电阻率值<200 m表示高孔隙率,高黏土含量和高饱和度,这是在大坝设计中需要认真考虑的土壤条件的指标。

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