通过原位测试确定粒状土的约束模量--第 1 部分分析

K. Massarsch
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摘要

评估约束模量是计算粒状土沉降的关键步骤。本文介绍了如何通过地震试验得出约束模量的新概念。本文探讨了地震实验室和现场试验的优势和局限性。在全面回顾实验室共振柱和扭剪试验的基础上,定量定义了影响剪切模量的最重要参数,如剪切应变和约束应力。此外,将剪切模量转换为约束模量所需的泊松比也与应变有关。本文提出了一种经验关系,根据这种关系,可以在较宽的应变范围(10-4-10-0.5%)内用数值定义切向剪切模量随剪切应变的变化。切线剪切模量是通过微分正切剪切模量得到的。根据切线模量概念,切线约束模量受模量数 m 和应力指数 j 的制约。回顾了粒状土的实验室测试结果,根据这些结果可以估算原始加载和卸载/重载时的模量数。还提出了小应变剪切模量 G0 与模量数 m 之间的相关性。模量数也可通过静态锥入试验得出,前提是锥阻力根据平均有效应力进行了调整。在另一篇论文中,本文提出的概念被应用于一个实验场地的数据,该实验场地进行了不同类型的地震试验和锥入试验。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Determination of Constrained Modulus of Granular Soil from In Situ Tests—Part 1 Analyses
Assessing the constrained modulus is a critical step in calculating settlements in granular soils. This paper describes a novel concept of how the constrained modulus can be derived from seismic tests. The advantages and limitations of seismic laboratory and field tests are addressed. Based on a comprehensive review of laboratory resonant column and torsional shear tests, the most important parameters affecting the shear modulus, such as shear strain and confining stress, are defined quantitatively. Also, Poisson’s ratio, which is needed to convert shear modulus to constrained modulus, is strain-dependent. An empirical relationship is presented from which the variation in the secant shear modulus with shear strain can be defined numerically within a broad strain range (10−4–10−0.5%). The tangent shear modulus was obtained by differentiating the secant shear modulus. According to the tangent modulus concept, the tangent constrained modulus is governed by the modulus number, m, and the stress exponent, j. Laboratory test results on granular soils are reviewed, based on which it is possible to estimate the modulus number during virgin loading and unloading/reloading. A correlation is proposed between the small-strain shear modulus, G0, and the modulus number, m. The modulus number can also be derived from static cone penetration tests, provided that the cone resistance is adjusted with respect to the mean effective stress. In a companion paper, the concepts presented in this paper are applied to data from an experimental site, where different types of seismic tests and cone penetration tests were performed.
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