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Deformation characteristics of bedded sandstone in uniaxial compression

机译:层状砂岩单轴压缩变形特性

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A series of uniaxial compressive strength tests were performed to study the deformation characteristics of bedded sandstone with bedding layers in different orientations.Test results revealed that the samples with bedding layers oriented in smaller angles (55°,35°,20°,and 10°),measured from the horizontal axis,undergo larger deformations compared to that of the samples with bedding layers oriented in higher angles (83°)at any stage of loading.When 75% of the peak load is reached,a considerable deformation had taken place in samples with bedding layers oriented in smaller angles (55°,35°,20°,and 10°),whereas a significantly less deformation had taken place in samples with bedding layers oriented in higher angles (83°).Moreover,at 55°and 35° bedding orientations,deformation was mainly observed within the middle region of specimens and at 20° and 10° bedding orientations deformation was more diffused throughout the specimen.
机译:进行了一系列单轴抗压强度试验,研究了层状砂岩在不同方向上的变形特性,试验结果表明,层状砂岩样品的取向角度较小(55°,35°,20°和10°)。 ),从水平轴测量,在任何加载阶段,与具有较高角度(83°)的地层的样品相比,其变形都更大。当达到峰值载荷的75%时,发生了相当大的变形在具有较小角度(55°,35°,20°和10°)的床上用品的样品中,在具有较大角度(83°)的床上用品的样品中发生的变形明显更少。此外,在55°在顺层和偏向35°层理方向上,变形主要发生在试样的中部区域,在顺层和偏向20°和10°取向下,变形在整个样品中更加分散。

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