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Three-dimensional fractal distribution of the number of rock-mass fracture surfaces and its simulation technology

机译:岩体断裂面数量的三维分形分布及其模拟技术

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摘要

The number of rock-mass fractures obeys a fractal distribution. In this study, numerical simulation was performed to confirm that the number of rock-mass fracture surfaces also obeys a three-dimensional fractal distribution. A simulation model is proposed here for the three-dimensional fractal distribution of the number of rock-mass fracture surfaces. Random distributions of fracture surfaces (RDFS) can be divided into three types: heavy random, weakly random, and distributed by group. By extensive calculations and theoretical deduction, the relation of the three types RDFS between the 3D fractal dimension (D-s) of the fracture surfaces and the fractal parameter (D-L) of the fracture trajectory in a 2D profile, D-L = D-s - 1, has been derived. It has further been proved that the 2D fractal dimension (D-L) is not related to the initial value of the fracture-surface distribution. The initial value of the 2D fractal distribution (N-L) shows a linear relation with the initial value of the 3D fractal distribution (N-s), N-L = kNs, where k is determined by the projection relation between the rock-mass profile and the 3D fracture surface.
机译:岩体裂缝的数量服从分形分布。在这项研究中,进行了数值模拟,以确认岩体断裂面的数量也服从三维分形分布。这里提出了一个模拟模型,用于岩体断裂面数量的三维分形分布。断裂面的随机分布(RDFS)可以分为三种类型:重随机,弱随机和按组分布。通过大量的计算和理论推论,已经确定了三种类型的RDFS在2D轮廓DL = Ds-1中的断裂表面的3D分形维数(Ds)与断裂轨迹的分形参数(DL)之间的关系。派生。进一步证明了二维分形维数(D-L)与断裂面分布的初始值无关。 2D分形分布(NL)的初始值与3D分形分布(Ns)的初始值呈线性关系,NL = kNs,其中k由岩体轮廓与3D裂缝之间的投影关系确定表面。

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