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ATwo-dimensional Mono-fractal Approach to Natural Fracture Networks in Rocks

机译:岩石自然断裂网络的二维单分形方法

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摘要

The mono-fractal dimension and geometric features of outcropping fractures in welded tuff and tuffaceous mudstone, and aritifcial 2D network models have been investigated. The fractal dimension of observed fracture sets were determined using the box-counting method, and several geometric characteristics including length distribution, orientation, connectivity, number of fractures, and total length of fractures were quantified in order to construct a two-dimensional fracture network model. The space filling fracturing of a welded tuff was represented by a single fractal dimension from 1.6mm through 10 m square scales, however, an universal fractal property could not be observed in the case of tuffaceous mudstone in spite of fractal behavior at each scale. These differences of fractal features between the welded tuff and the tuffaceous mudstone are considered to be related to the mechanism of fracture generation and different fracture mechanical characteristics. Computer-generated two-dimensional fracture network patterns of the welded tuff utilizing the observed fractal dimension and geometric relationship have been found capable of simulating the natural fracture patterns. This artificial model, which is founded on the uniform fractal property of a given fracture set from microscopic to 10 m scales in the welded tuff, is capable of being expanded to larger scales on the basis of self-similarity.
机译:研究了凝灰岩和凝灰质泥岩中露头裂缝的单分形维数和几何特征,以及人工二维网络模型。使用盒数法确定观察到的裂缝组的分形维数,并量化包括长度分布,取向,连通性,裂缝数和裂缝总长度在内的几个几何特征,以构建二维裂缝网络模型。凝灰岩的空间填充裂缝由1.6mm到10m平方尺的单个分形维数表示,但是,尽管在每个尺度上都有分形行为,但在凝灰质泥岩中却没有观察到普遍的分形特性。焊接凝灰岩和凝灰质泥岩之间的分形特征差异被认为与裂缝产生的机理和不同的断裂力学特性有关。已经发现利用观察到的分形维数和几何关系的计算机生成的焊接凝灰岩的二维断裂网络模式能够模拟自然断裂模式。该人工模型基于焊接凝灰岩中从微观到10 m尺度的给定裂缝组的均匀分形特性,能够基于自相似性将其扩展到更大尺度。

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