谭罗荣. 2002: 黄土孔隙结构的分形特征与湿陷性关系的探讨. 工程地质学报, 10(S1): 427-431.
    引用本文: 谭罗荣. 2002: 黄土孔隙结构的分形特征与湿陷性关系的探讨. 工程地质学报, 10(S1): 427-431.
    TAN Luorong. 2002: A STUDY OF RELATIONSHIP BETWEEN COLLAPSIBILITY OF LCOESS AND ITS FRACTAL CHARACTER OF PORE STRUCTURE. JOURNAL OF ENGINEERING GEOLOGY, 10(S1): 427-431.
    Citation: TAN Luorong. 2002: A STUDY OF RELATIONSHIP BETWEEN COLLAPSIBILITY OF LCOESS AND ITS FRACTAL CHARACTER OF PORE STRUCTURE. JOURNAL OF ENGINEERING GEOLOGY, 10(S1): 427-431.

    黄土孔隙结构的分形特征与湿陷性关系的探讨

    A STUDY OF RELATIONSHIP BETWEEN COLLAPSIBILITY OF LCOESS AND ITS FRACTAL CHARACTER OF PORE STRUCTURE

    • 摘要: 根据已有的资料,探讨了黄土孔隙结构的分形特征,定义了分形特征孔隙半径r2,讨论了分形特征与湿陷性的关系。结果表明,分形特征半径r:与湿陷性具有良好的线性关系,分维值Dx可以反映黄土剖面的成土地质年代。

       

      Abstract: On the basis of publicized data, the fractal chracter of pore structure in loess is studied, are also deter-mined fractal characteristic pore radius r2 and discussed relationship between fractal character values and collapsi-bility,results show that there are a good liner relatiouship between r2 and collapsibility, and fractal dimension D2 can reflected geological age of loess section.

       

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