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谢和平, 王金安. 岩石节理(断裂)表面的多重分形性质[J]. 力学学报, 1998, 30(3): 314-320. DOI: 10.6052/0459-1879-1998-3-1995-132
引用本文: 谢和平, 王金安. 岩石节理(断裂)表面的多重分形性质[J]. 力学学报, 1998, 30(3): 314-320. DOI: 10.6052/0459-1879-1998-3-1995-132
MULTIFRACTAL BEHAVIORS OF FRACTURE SURFACES IN ROCKS 1)[J]. Chinese Journal of Theoretical and Applied Mechanics, 1998, 30(3): 314-320. DOI: 10.6052/0459-1879-1998-3-1995-132
Citation: MULTIFRACTAL BEHAVIORS OF FRACTURE SURFACES IN ROCKS 1)[J]. Chinese Journal of Theoretical and Applied Mechanics, 1998, 30(3): 314-320. DOI: 10.6052/0459-1879-1998-3-1995-132

岩石节理(断裂)表面的多重分形性质

MULTIFRACTAL BEHAVIORS OF FRACTURE SURFACES IN ROCKS 1)

  • 摘要: 提出了新的投影覆盖法———ProjectiveCoveringMethod(PCM),并结合无接触激光表面测量技术直接测定出断裂表面分维值D∈[2,3).建立了表面粗糙性投影覆盖概率函数,分析了节理(断裂)表面的多重分形性质.

     

    Abstract: Following fractal geometry introduced by B.B. Mandelbrot,many researchers have described quantitatively the roughness of fractured surfaces and also tried to establish the relationship between the fractal dimension and mechanical parameters. Extensive experiments and measurement show that, to some extent, fracture surfaces in rocks exhibit statistical fractal behavior in a certain range of scale. In fact, understanding of fractal behavior of fracture surfaces advances step by step. Initially, people paid at...

     

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