黝帘石-乌云石在单轴和三轴压缩条件下的物理和机械特性研究

N.N. Kuznetcov, A.K. Pak
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摘要

对岩体变形和破坏过程的研究通常是在实验室条件下对样品进行的。为此,我们使用了广泛使用的试验设备,这些设备可以创造与岩体内部类似的加载条件。基本上,加载模式是只在样品的一侧(沿一条轴线)施加力,即单轴压缩或拉伸。可以沿三个轴施加载荷的测试设备,即三轴压缩,使用较少。这种设备通常非常昂贵,而且测试需要大量的时间和资源。然而,这种加载模式是最有趣的模式之一,因为它接近岩体的真实情况。本文介绍了在单轴和三轴压缩条件下对黝帘石-乌云岩样本(科拉地区基比尼丘陵的岩石)进行实验研究的结果。研究的目的是确定这种岩石的抗压强度值如何变化,评估特定应变能的临界值,以及从单轴加载模式过渡到三轴加载模式期间的动态破坏趋势。实验研究表明,在三轴压缩条件下,黝帘石-乌云岩样本的抗压强度值和比应变能临界值比在单轴压缩条件下增加得更快。研究结果表明,所研究的岩石在单轴压缩条件下容易发生动态破坏,而在三轴压缩条件下则保持了这种破坏趋势。
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Investigation of physical and mechanical properties of ijolite-urtite under uniaxial and triaxial compression
The study of deformation and failure processes in rock masses is often carried out in laboratory conditions on samples. Widely used test equipment is used for this purpose, which makes it possible to create loading conditions similar to those inside the rock mass. Basically, the loading mode is implemented when forces are applied only to one side of the sample (along one axis), that is, uniaxial compression or tension. Test equipment that allows creation of loading along three axes, i.e. triaxial compression, is used less frequently. Such equipment is often very expensive, and testing requires a lot of time and resources. Nevertheless, this loading mode is one of the most interesting, since it is close to real conditions in the rock mass. This paper presents the results of experimental studies of ijolite-urtite samples (rocks from the Khibiny massif, the Kola Region) in conditions of uniaxial and triaxial compression. The purpose of the research is to establish how the values of the compressive strength of this rock change, to assess the critical values of the specific strain energy, as well as the tendency to dynamic destruction during the transition from the uniaxial loading mode to the triaxial one. The experimental studies revealed that there exists a sharper increase in the values of compressive strength and the critical values of specific strain energy of the ijolite-urtite samples in conditions of triaxial compression than under uniaxial compression. It has been established that the studied rock is prone to dynamic failure under uniaxial compression and preserve its tendency to this type of failure under triaxial compression.
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