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DISCUSSION ON THE RELATION BETWEEN FRACTAL DISTRIBUTION OF SLOPE LOOSE DEPOSIT AND ITS MECHANICS PRINCIPLE

机译:边坡松散沉积物分形分布与力学原理的关系探讨。

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摘要

The fractal law of loose slope deposits around the State Road 317 Dujiangyan to Wenchuan,was studied by employing fractal theory. The research shows that: The fractal dimension of particle size distribution of the slope loose deposit is between 2 and 3.Density,porosity and internal friction angle was studied experimentally with large relative densitometer and direct shear apparatus. The result shows that,as fractal dimension increases,density and porosity of the slope loose deposits increases,while the internal friction angle decreases.On this basis,a fitted formula which can approximately reflect the relation between fractal dimension,density,porosity and internal friction angle was obtained.
机译:运用分形理论研究了都江堰317国道至汶川周围松散堆积物的分形规律。研究表明:边坡疏松沉积物粒度分布的分形维数在2〜3之间。采用大的相对密度仪和直接剪切装置对密度,孔隙率和内摩擦角进行了实验研究。结果表明,随着分形维数的增加,边坡疏松沉积物的密度和孔隙率增加,内摩擦角减小。在此基础上,拟合方程可以近似地反映分形维数,密度,孔隙率与内摩擦之间的关系。获得角度。

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