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3-D distribution of tensile stress in rock specimens for the Brazilian test

机译:巴西测试中岩石样品中拉应力的3-D分布

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摘要

It is claimed that the formula used for calculating the tensile strength of a disk-shaped rock specimen in the Brazilian test is not accurate, because the formula is based on the 2-dimensional elastic theory and only suitable for very long or very short cylinders. The Matlab software was used to obtain the 2-dimensional distribution of stress in the rock specimen for Brazilian test. Then the 2-dimensional stress distribution in Brazilian disk was analyzed by the Marc FEM software. It can be found that the results obtained by the two software packages can verify each other. Finally, the 3-dimensional elastic stress in the specimen was calculated. The results demonstrate that the distribution of stress on the cross section of the specimen is similar to that in 2-dimension, However, the value of the stress on the cross section varies along the thickness of the specimen and the stress is bigger when getting closer to the end of the specimen. For the specimen with a height-to-diameter ratio of 1 and a Poisson's ratio of 0.25, the tensile strength calculated with the classical 2-D formula is 23.3 percent smaller than the real strength. Therefore, the classical 2-D formula is too conservative.
机译:据称,在巴西测试中用于计算盘状岩石试样抗拉强度的公式不准确,因为该公式基于二维弹性理论,并且仅适用于非常长或非常短的圆柱体。用Matlab软件获得岩石样品中二维应力分布,用于巴西测试。然后使用Marc FEM软件分析巴西圆盘中的二维应力分布。可以发现,两个软件包得到的结果可以相互验证。最后,计算样品中的三维弹性应力。结果表明,试样截面上的应力分布与二维应力分布相似,但是截面上的应力值随试样厚度的变化而变化,靠近时应力更大。到样品的末端。对于高径比为1且泊松比为0.25的样品,用经典二维公式计算的抗拉强度比实际强度小23.3%。因此,经典的二维公式过于保守。

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