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Deformation characteristics of lacustrine carbonate silt in the Julian Alps

机译:朱利安阿尔卑斯山湖相碳酸盐粉砂的变形特征

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The deformation characteristics, shear moduli and damping ratios of reconstituted lacustrine carbonate silt samples were investigated in different kinds of laboratory tests. Material from a landslide that occurred in a seismically very active area in Slovenia was used in the tests. The initial values of this material's deformation characteristics and the extent to which these values change due to increasing shear strain depend on a number of factors, such as the degree of saturation, the initial void ratio, over-consolidation, and the effective stresses. The use of a volumetric threshold strain has proved to be the best way of describing the shear modulus reduction curve irrespective of any other factors, and it fits well with the data obtained in the experiments. The critical state and consolidation lines for the investigated material are presented in the paper as deformational characteristics at critical strain levels. The material's liquefaction potential was studied for certain in situ conditions.
机译:在不同的实验室测试中,研究了再生的湖相碳酸盐粉砂样品的变形特性,剪切模量和阻尼比。测试使用了发生在斯洛文尼亚地震活跃地区的滑坡材料。该材料的变形特性的初始值以及由于剪切应变增加而导致的这些值变化的程度取决于许多因素,例如饱和度,初始空隙率,过度固结和有效应力。事实证明,使用体积阈值应变是描述剪切模量降低曲线的最佳方法,而与其他任何因素无关,它与实验中获得的数据非常吻合。在本文中,被研究材料的临界状态和固结线作为临界应变水平下的变形特征呈现。在某些原位条件下研究了材料的液化潜力。

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