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Shaking table tests to investigate the influence of various factors on the liquefaction resistance of sands

机译:振动台试验以研究各种因素对砂土抗液化性的影响

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This paper presents the shaking table studies to investigate the factors that influence the liquefaction resistance of sand. A uniaxial shaking table with a perspex model container was used for the model tests, and saturated sand beds were prepared using wet pluviation method. The models were subjected to horizontal base shaking, and the variation of pore water pressure was measured. Three series of tests varying the acceleration and frequency of base shaking and density of the soil were carried out on sand beds simulating free field condition. Liquefaction was visualized in some model tests, which was also established through pore water pressure ratios. Effective stress was calculated at the point of pore water pressure measurement, and the number of cycles required to liquefy the sand bed were estimated and matched with visual observations. It was observed that there was a gradual variation in pore water pressure with change in base acceleration at a given frequency of shaking. The variation in pore water pressure is not significant for the range of frequency used in the tests. The frequency of base shaking at which the sand starts to liquefy when the sand bed is subjected to any specific base acceleration depends on the density of sand, and it was observed that the sand does not liquefy at any other frequency less than this. A substantial improvement in liquefaction resistance of the sand was observed with the increase in soil density, inferring that soil densification is a simple technique that can be applied to increase the liquefaction resistance
机译:本文介绍了振动台研究,以研究影响砂土抗液化性的因素。使用带有有机玻璃模型容器的单轴振动台进行模型测试,并使用湿法浸没法制备饱和砂床。对模型进行水平基础摇动,并测量孔隙水压力的变化。在模拟自由场条件的沙床上进行了三个系列的测试,这些测试改变了基础振动的加速度和频率以及土壤的密度。在一些模型测试中可以看到液化,这也可以通过孔隙水压力比来确定。在孔隙水压力测量时计算有效应力,并估算液化砂床所需的循环次数,并与目视观察相匹配。观察到,在给定的振动频率下,孔隙水压力会随着基础加速度的变化而逐渐变化。在测试中使用的频率范围内,孔隙水压力的变化并不明显。当砂床受到任何特定的基础加速度时,砂开始液化的基础振动的频率取决于砂的密度,并且观察到,在低于此的任何其他频率下,砂都不会液化。随着土壤密度的增加,沙土的抗液化性有了实质性的改善,这表明土壤致密化是一种可以用来提高抗液化性的简单技术。

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