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Experimental investigation of the strength and failure behavior of layered sandstone under uniaxial compression and Brazilian testing

机译:层状砂岩单轴压缩强度和破坏行为的试验研究及巴西试验

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As a typical inherently anisotropic rock, layered sandstones can differ from each other in several aspects, including grain size, type of material, type of cementation, and degree of compaction. An experimental study is essential to obtain and convictive evidence to characterize the mechanical behavior of such rock. In this paper, the mechanical behavior of a layered sandstone from Xuzhou, China, is investigated under uniaxial compression and Brazilian test conditions. The loading tests are conducted on 7 sets of bedding inclinations, which are defined as the angle between the bedding plane and horizontal direction. The uniaxial compression strength (UCS) and elastic modulus values show an undulatory variation when the bedding inclination increases. The overall trend of the UCS and elastic modulus values with bedding inclination is decreasing. The BTS value decreases with respect to the bedding inclination and the overall trend of it is approximating a linear variation. The 3D digital high-speed camera images reveal that the failure and fracture of a specimen are related to the surface deformation. Layered sandstone tested under uniaxial compression does not show a typical failure mode, although shear slip along the bedding plane occurs at high bedding inclinations. Strain gauge readings during the Brazilian tests indicate that the normal stress on the bedding plane transforms from compression to tension as the bedding inclination increases. The stress parallel to the bedding plane in a rock material transforms from tension to compression and agrees well with the fracture patterns; a??central fracturesa?? occur at bedding inclinations of 0?°a??75?°, a??layer activationa?? occurs at high bedding inclinations of 75?°a??90?°, and a combination of the two occurs at 75?°.
机译:作为一种典型的固有各向异性岩石,层状砂岩在几个方面可能会有所不同,包括粒度,材料类型,胶结类型和压实度。为了获得定性证据来表征此类岩石的力学行为,必须进行实验研究。本文在单轴压缩和巴西试验条件下研究了来自中国徐州的层状砂岩的力学行为。对7组床上用品倾斜度进行载荷测试,这些倾斜度定义为床上用品平面与水平方向之间的角度。当垫层倾角增加时,单轴抗压强度(UCS)和弹性模量值显示波动性变化。 UCS和弹性模量值随层间倾斜度的总体趋势正在下降。 BTS值相对于床上用品倾斜度降低,并且其总体趋势接近线性变化。 3D数字高速相机图像显示出样品的破坏和断裂与表面变形有关。尽管在较高的层理倾角下会发生沿层理面的剪切滑移,但在单轴压缩下测试的层状砂岩并未显示出典型的破坏模式。巴西测试期间的应变片读数表明,随着层理倾斜度的增加,层理平面上的法向应力从压缩转变为张紧。岩石材料中平行于顺层平面的应力从拉力转变为压缩力,并与裂缝形态吻合。中央骨折发生在顺层倾角为0°a ?? 75°?,层激活a?发生在75°a≤90°的高层倾角上,而两者的结合发生在75°a。

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