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Preliminary Determination of Subsurface Soil Profiles in Akenfa Community, Bayelsa State, Nigeria

机译:尼日利亚巴耶尔萨州阿肯法社区地下土壤剖面的初步确定

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摘要

This study aims at establishing the sub-soil types and profile to ascertain the geotechnical characteristics of the underlying soils in Akenfa in Yenagoa, Yenagoa Local Government Area of Bayelsa State, Nigeria and recommend appropriate foundation design and construction of projects in the area. Three (3) geotechnical boreholes were drilled at the site to obtain baseline data on geotechnical properties of the soil and water level monitoring, the boreholes were advanced with the use of a cable percussion boring rig and were terminated to a maximum depth of 30m. The particle size distributions of a number of representative samples of the cohesionless soils were determined by sieve analysis. The results show that the samples are low to medium plasticity silty clay. The lithology revealed intercalations of clay and sand in thin layers to a depth of 2.0m below the existing ground level. Underlying this clay is a stratum of loose to medium dense sand and dense sand. The sand is well sorted grading from fine to medium as the borehole advances. The laboratory analysis showed that the silty clay has undrained shear strength of 48 kPa. The loose sand has a maximum SPT (N) value of 12 while the medium dense sand has maximum SPT (N) value of 28. Considering the nature of the civil structures to be sited in the area, it is anticipated the load and the moderate compressibility of this near surface silty clay and the underlying loose silty sand be supported by means of raft foundation founded within the clay layer. It is recommended that studies on the geotechnical characteristics of the area be carried out as it provides valuable data that can be used for foundation design and other forms of construction for civil engineering structures in order to minimize adverse effects and prevention of post construction problems.
机译:这项研究的目的是确定亚土的类型和剖面,以确定在尼日利亚巴耶尔萨州的耶拿哥地方政府地区耶拿哥的阿肯法下层土壤的岩土特性,并建议该地区适当的基础设计和项目建设。在现场钻了三(3)个岩土工程钻孔,以获取有关土壤和水位监测的岩土工程性能的基准数据,并使用电缆冲击钻机推进钻孔,并将钻孔终止至最大深度30m。通过筛分分析确定了许多无粘性土壤代表性样品的粒径分布。结果表明,样品为中低塑性粉质粘土。岩性揭示了粘土和沙子在薄层中的插入,其深度低于现有地面的2.0m。在该粘土的下面是疏松至中等致密砂和致密砂的地层。随着井眼的推进,砂子的分类从细到中等的分级。实验室分析表明,粉质粘土的不排水剪切强度为48 kPa。疏松砂的最大SPT(N)值为12,而中密度砂的最大SPT(N)值为28。考虑到将要放置在该区域的土木结构的性质,可以预期载荷和中等强度这种近地表粉质粘土和下面的松散粉质砂的可压缩性通过在粘土层中建立的筏板基础来支撑。建议对该区域的岩土特征进行研究,因为它提供了可用于基础设计和土木工程结构其他形式的施工的有价值的数据,以最大程度地减少不利影响并防止后期施工问题。

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