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Cyclic strength of imperfectly saturated sands and analysis of liquefaction

机译:不完全饱和砂土的循环强度和液化分析

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The simplified method of analysis to assess liquefaction potential of a given sand deposit is briefly introduced in the first part of this paper. Then, recent advances in the laboratory testing for evaluating liquefaction resistance are described with a particular emphasis on the sand partly saturated with water. As a means to identify the degree of saturation which is applicable for both field deposits and laboratory samples, the use of the longitudinal wave (P-wave) is proposed based on a suite of data obtained from the triaxial tests in the laboratory. It is recommended that the non-destructive P-wave measurements be carried out first to determine the degree of saturation, and then the cyclic triaxial tests involving large destructive strains should be performed to determine the cyclic strength on the same sample of the sand. In order to demonstrate usefulness of the proposed approach, two sets of undisturbed samples were secured from two sites; one is located in Sakai-minato city which has suffered severe liquefaction at the time of the 2000 Tottoriken-Seibu earthquake and the other site is located in Koshigaya city, Saitama, where likelihood of liquefaction to occur in a future earthquake is of major concern. Penetration tests and in-situ velocity logging were also conducted at these two sites. By adjusting the P-wave velocity of the undisturbed samples in the laboratory so as to have the same velocity in the field, the in-situ state of saturation was reproduced in the laboratory samples. Then, the cyclic loading tests were conducted to determine the cyclic strength of intact samples. The results of the laboratory tests as above were incorporated into the simple method of liquefaction analysis described in the first section of this paper. The analysis seems to yield results which are in reasonably good agreement with what was observed at the time of the earthquake. (Communicated by Toshio SAWADA, M.J.A.)
机译:本文的第一部分简要介绍了评估给定砂土液化潜力的简化分析方法。然后,描述了用于评估抗液化性的实验室测试的最新进展,其中特别强调了部分被水饱和的沙子。作为确定适用于田间沉积物和实验室样品的饱和度的一种方法,基于从实验室三轴测试获得的一组数据,提出了使用纵波(P波)的方法。建议先进行无损P波测量以确定饱和度,然后再进行涉及大破坏应变的循环三轴试验,以确定同一砂样的循环强度。为了证明所提出方法的有效性,从两个位置固定了两组不受干扰的样本。一个地点位于Sa都港市,在2000年鸟取前西武地震时遭受了严重的液化,另一地点位于ita玉县越谷市,这是未来地震发生的可能性。在这两个地点也进行了渗透测试和原位速度测井。通过调节实验室中未扰动样品的P波速度,使其在野外具有相同的速度,就可以在实验室样品中恢复原位饱和状态。然后,进行循环载荷测试以确定完整样品的循环强度。上述实验室测试的结果已纳入本文第一部分所述的简单液化分析方法中。该分析似乎得出的结果与地震发生时观察到的结果相当吻合。 (由M.J.A.佐渡敏夫(Toshio SAWADA)通讯)

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