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A Soil Structure Index to Predict Rate Dependence of Stress-Strain Behavior

机译:一种土壤结构指标,以预测应力 - 应变行为的率依赖性

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Soil structure depends on a number of influences, including geomorphology, groundwater fluctuations and geochemistry. In the case of soft clays, this structure is believed to play a significant role in the degree of rate dependence of the clay's stress-strain behavior. However, there has been no systematic method developed to predict what degree of structure will produce a particular degree of stress-strain rate dependence. This paper presents a methodology based on Burland's (1990) void index (I_v) framework to predict the type of rate dependence that could be expected for a soil's stress-strain behavior in one-dimensional (1-D) compression. Three categories of rate dependence in 1-D compression have been reported in the literature, characterized by the following: 1) rate dependence in both the preconsolidation stress (σ'p) and virgin compression; 2) σ'p is not rate dependent, but the slope of the virgin compression line varies with strain rate; and 3) little or no rate dependence in any portion of the compression curve. Based on a series of 1-D tests on soils from Canada and the U.S., rate-dependent behavior types were compared to each soil's natural state in Burland's I-v versus vertical effective stress space. A so-called "structure number" (SN) is introduced, indicating how far the soil's natural state is from its intrinsic or remolded compression curve (ICL; SN = 0) and its original sedimentation compression curve (SCL; SN = 1). The contour with SN=2 is parallel to these two, approximately parallel lines, but above the SCL at a distance equal to the SCL-ICL gap. Higher SN value contours are similarly obtained. The results indicate that SN correlates well to the type of rate dependence observed in the 1-D compression tests. These initial results appear to provide a rational link between soil structure and strain rate dependence.
机译:土壤结构取决于多种影响,包括地貌,地下水波动和地球化学。在软粘土的情况下,认为这种结构在粘土的应力 - 应变行为的速率依赖性程度上发挥着重要作用。然而,没有开发系统的方法以预测结构程度将产生特定的应力 - 应变率依赖性。本文提出了一种基于Burland(1990)空隙指数(I_V)框架的方法,以预测可以在一维(1-D)压缩中的土壤应力 - 应变行为的速率依赖性的类型。在文献中报道了三类1-D压缩中的速率依赖性,其特征在于以下:1)依赖于前透镜应力(ΣP)和处女压缩; 2)ΣP不依赖于速率,但初始压缩线的斜率随应变速率而变化; 3)在压缩曲线的任何部分中少于或没有速率依赖性。基于来自加拿大和美国的土壤的一系列1-D测试,将富裕的行为类型进行比较,每个土壤在伯兰I-V的I-V与垂直有效应力空间中的自然状态。介绍了所谓的“结构编号”(SN),表明土壤的自然状态是从其内在或重折叠的压缩曲线(ICL; SN = 0)及其原始沉降压缩曲线(SCL; SN = 1)的距离。 SN = 2的轮廓与这两个近似平行线平行,但是在SCL上方等于SCL-ICL间隙的距离。类似地获得了较高的Sn值轮廓。结果表明,SN与在1-D压缩测试中观察到的速率依赖性的类型相关。这些初始结果似乎提供了土壤结构和应变率依赖之间的合理联系。

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