The use of critical state soil mechanics to characterise Christchurch soil in relation to liquefaction susceptibility

Jeremy Tan, Rolando P Orense, A. O’Sullivan
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Abstract

The majority of current procedures used to deduce liquefaction potential of soils rely on empirical methods. These methods have been proven to work in the past, but these methods are known to overestimate the liquefaction potential in certain regions of Christchurch due to a whole range of factors, and the theoretical basis behind these methods cannot be explained scientifically. Critical state soil mechanics theory was chosen to provide an explanation for the soil’s behaviour during the undrained shearing. Soils from two sites in Christchurch were characterised at regular intervals for the critical layers and tested for the critical state lines (CSL). Various models and relationships were then used to predict the CSL and compared with the actual CSL. However none of the methods used managed to predict the CSL accurately, and a separate Christchurch exclusive relationship was proposed. The resultant state parameter values could be obtained from shear-wave velocity plots and were then developed into cyclic resistance ratios (CRR). These were subsequently compared with cyclic stress ratios (CSR) from recent Christchurch earthquakes to obtain the factor of safety. This CSL-based approach was compared with other empirical methods and was shown to yield a favourable relationship with visual observations at the sites’ locations following the earthquake.
使用临界状态土力学来表征基督城土壤的液化敏感性
目前用于推断土壤液化潜力的大多数程序依赖于经验方法。这些方法在过去已经被证明是有效的,但由于一系列因素,这些方法被认为高估了基督城某些地区的液化潜力,这些方法背后的理论基础无法科学地解释。采用临界状态土力学理论对不排水剪切过程中土体的行为进行了解释。对基督城两个地点的土壤进行了定期的临界层特征和临界状态线(CSL)测试。然后利用各种模型和关系预测CSL,并与实际CSL进行比较。然而,所使用的方法都无法准确预测CSL,并且提出了一个单独的基督城专属关系。由此得到的状态参数值可由剪切波速图得到,然后发展为循环阻力比(CRR)。随后将这些数据与最近基督城地震的循环应力比(CSR)进行比较,以获得安全系数。将这种基于csl的方法与其他经验方法进行了比较,并显示出与地震后在站点位置的目视观测产生良好的关系。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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