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首页> 外文期刊>Asian journal of earth sciences >Determination of the Bearing Capacities of Sandstone and Shale Lithologies from Shear Wave Velocity in the Niger Delta Sedimentary Basin, Nigeria
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Determination of the Bearing Capacities of Sandstone and Shale Lithologies from Shear Wave Velocity in the Niger Delta Sedimentary Basin, Nigeria

机译:从尼日利亚尼日尔三角洲沉积盆地的剪切波速度确定砂岩和页岩岩性的承载能力

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摘要

The bearing capacities and coefficient of subgrade reaction of sand and shale lithologies of Niger Delta sedimentary basin, Nigeria have been computed from shear wave velocities using a relatively simple formula. The shear velocities were obtained from five oil exploratory wells. The computed ultimate bearing capacities of the sand ranges from 3141.755 to 5593.447 kN m~(-3) with an average of 4367.601 kN m~(-3) while, that of the shale ranges between 2487.786 and 6335.588 kN m~(-3) with an average of 4411.687 kN m~(-3). The computed allowable bearing capacity of the sand varies from 1047.252 to 1864.482 kN m~(-3) while that of the shale lithology is from 829.262 to 2111.863 kN m~(-3). Furthermore, the estimated subgrade reaction for the sand varies between 41890.07 and 74579.29 kN m~(-3) while that of the shale is from 33170.48 to 84474.5 kN m~(-3). The results show that the bearing capacities of the sand and shale lithologies are very high. This may be attributed to high consolidation and compaction of the formations in the subsurface and thereby resulting in the stability of most foundations in the area. Although, the shale lithology has a high bearing capacities and coefficient of subgrade reaction yet it is not advisable to put foundation on it whenever it is close to the earth surface because when it has the ability to swell/contract whenever it absorb or looses water it.
机译:尼日利亚尼日尔三角洲沉积盆地的砂岩和页岩岩性的承载力和路基反应系数是使用一个相对简单的公式根据剪切波速度计算得出的。剪切速度是从五个探油井获得的。砂的计算极限承载力范围为3141.755至5593.447 kN m〜(-3),平均为4367.601 kN m〜(-3),而页岩的极限承载力为2487.786至6335.588 kN m〜(-3)平均为4411.687 kN m〜(-3)计算得到的砂的容许承载力为1047.252至1864.482 kN m〜(-3),而页岩岩性的容许承载力为829.262至2111.863 kN m〜(-3)。此外,估计的砂土路基反应在41890.07和74579.29 kN m〜(-3)之间变化,而页岩的路基反应从33170.48到84474.5 kN m〜(-3)。结果表明,砂岩和页岩岩性的承载力非常高。这可能归因于地下地下岩层的高度固结和压实,从而导致该地区大多数地基的稳定性。尽管页岩岩性具有较高的承载能力和路基反应系数,但不建议在靠近地表时就在其上打基础,因为只要它能够吸收或疏散水而发生膨胀/收缩, 。

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