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Research on the Development Mechanism of Postpeak Cracks in Sandstone under Different Confining Pressures

机译:不同施加压力下砂岩裂缝裂缝的发展机理研究

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Water inrush happens occasionally during deeper roadways excavation. It is mainly due to the lack of understanding in the formation and development mechanism of cracks and its spatial distribution pattern under ground stress. In view of this, this paper used different stress levels to represent the fracture state of different parts of the surrounding rock of the deep roadway; CT detection technique is used to scan the fractured sandstone in the postpeak state; and the CT images under different confining pressures are thus obtained. The geometrical parameters such as area, length, and width of the crack are used to describe the distribution patterns based on CT images processing technique and statistical principle. These patterns are then analyzed under varying postpeak stress levels and confining pressures. The result shows that, as the area, length, and width of the cracks get larger, number of cracks increases with decreasing stress level; at different stress levels, sandstone crack area probability density, crack length probability density, and crack width probability density form exceptional, linear, and Gaussian distribution, respectively. The amount of confining pressure affects the size of cracks and the extent of expansion. This means that the higher the confining pressure is, the easier the internal crack will be penetrated and expanded and the bigger the cracks are, and the number of cracks gets lesser. Such research results can be used to describe the propagation and evolution law of cracks under different stress states of postpeak rock, which also provide an important basis for further analysis of its permeability and the stability of roadway surrounding rock.
机译:在更深入的道路挖掘过程中偶尔会发生潮流。主要是由于裂缝的形成和发展机制缺乏了解及其在地面应力下的空间分布模式。鉴于此,本文使用了不同的应力水平来代表深道围岩周围岩石的不同部分的断裂状态; CT检测技术用于扫描突出状态下的裂缝砂岩;由此获得了不同限制压力下的CT图像。裂缝的区域,长度和宽度等几何参数用于描述基于CT图像处理技术和统计原理的分布模式。然后在不同的蛋止应力水平和限制压力下分析这些图案。结果表明,作为裂缝的区域,长度和宽度变大,裂缝数量随着应力水平的降低而增加;在不同的应力水平下,砂岩裂纹区域概率密度,裂缝长度概率密度和裂缝宽度概率密度分别形成出色,线性和高斯分布。限制压力的量会影响裂缝的大小和膨胀程度。这意味着限制压力越高,内部裂缝将被渗透和扩展,裂缝的越大,裂缝的数量变小。这些研究结果可用于描述Postpak Rock的不同应力状态下的裂缝的传播和演化定律,这也为进一步分析其渗透性和围岩道路的稳定性提供了重要的基础。

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