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Fractal characteristic of fracture in glass or single crystals of quartz by 3D micro X-ray CT measurement

机译:通过3D显微X射线CT测量测量玻璃或石英单晶的断裂的分形特征

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We analyzed the fractal characteristic of fracture geometry of experimentally fractured borosilicaternglass and single crystals of quartz samples using 3D micro X-ray Computed Tomography (CT)rntechniques. The fracture experiments were performed at the confining pressure (P_c) of 300 MPa andrnuniaxial compression under nominal axial strain rate of 5.0×10~(-4)/s using a Griggs apparatus with arnlead confining medium. Then the space distributions of fractures using a Box-Counting method werernmeasured for each micro X-ray CT image sliced both perpendicular and parallel to the direction ofrnmaximum compressive stress (XY-planes, YZ-planes and ZX-planes. The space distributions ofrnfractures showed a power-law distribution. The scaling exponents (D_(BC)) of the correlation of thernfractures space distributions in YZ-planes and ZX-planes ranged uniformly. Otherwise D_(BC) of thernspace distributions of fracture patterns in XY-planes increased toward the sides of each sample,rnespecially D_(BC) of the the glass sample fractured at P_c = 300 Mpa (GLS-300) increased suddenly fromrn1.1 to 1.9 toward the highly fractured bottom side. The relation between D_(BC) of GLS-300 and thernlogarithm of the area distortion ε in XY-planes showed a positive correlation in the range of high arearndistortion ε > 1. The heterogeneous distribution of DBC possibly shows heterogeneous distribution ofrnfracture energy. DBC in the range of low area distortion ε < 1 showed the constant behaviors in thernrange of 1.1 < D(BC) < 1.2 and can be ragarded as the background D_(BC) by the elastic deformation beforernthe destruction. Our result implies the presence of heterogeneity in fracturing energy densityrndistribution even in highly homogeneous glass samples, which lay on the background DBC. Thereforernwe should consider the inhomogeneity and anisotropy of the fracture space distribution in case ofrncomparison with the fractal dimensions of different analyzing directions or locations.
机译:我们使用3D微型X射线计算机断层扫描(CT)技术分析了实验性断裂的硼硅玻璃和石英样品单晶的断裂几何形状的分形特征。断裂实验是在300 MPa的围压(P_c)和标称轴向应变率为5.0×10〜(-4)/ s的单轴压缩下,使用带有arnlead围压介质的Griggs装置进行的。然后,使用Box-Counting方法对垂直于和平行于最大压缩应力方向(XY平面,YZ平面和ZX平面)的X射线显微CT图像测量裂缝的空间分布。表现出幂律分布,YZ平面和ZX平面中裂隙空间分布相关性的标度指数(D_(BC))均匀变化,否则XY平面中裂隙模式的裂隙空间分布的D_(BC)增大朝着每个样品的侧面,尤其是在P_c = 300 Mpa(GLS-300)断裂的玻璃样品的D_(BC)朝着高度断裂的底面突然从rn1.1增加到1.9。 GLS-300与XY平面上的面积变形ε的热对数在高变形ε> 1的范围内呈正相关。DBC的非均质分布可能显示了断裂能的非均质分布。在低区域畸变ε<1的范围内,在1.1

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