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Three-dimensional Characteristics of the Loess's microstructure and comparison before and after collapse

机译:黄土微观结构的三维特征及崩塌前后的比较

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Microstructure surface undulation is an important parameter to denote the loess microstructure characteristics, but the current studies are mostly qualitative and quantitative two-dimensional analysis, which difficult to reflect the situation of soil microstructure surface undulation. Analysis based on the microstructure characteristics of loess in western Liaoning, translate the gray value which extracted from SEM image into the elevation data of loess microstructure surface, constitute the three-dimensional digital images of Loess's microstructure surface undulation before and after collapse, proposing SEM photographs three-dimensional visualization method and characterization parameters. This method is simple to implement, and can intuitively observe the structure of the Loess's microstructure surface undulation before and after collapse. Through improved projective covering method, calculate the loess's fractal dimension before collapse is 2.508, but 2.590 after collapse, this shows that loess after collapse, microstructure surface undulation extent is increased, and pore complexity extent significant increased.
机译:微结构表面起伏是表示黄土微结构特征的重要参数,但目前的研究大多是定性和定量的二维分析,难以反映土壤微结构表面起伏的情况。根据辽西黄土的微观结构特征进行分析,将扫描电镜图像中提取的灰度值转化为黄土微结构表面的高程数据,构成黄土微结构表面塌陷前后的三维数字图像,并提出SEM照片。三维可视化方法和特征参数。该方法易于实现,可以直观地观察崩塌前后黄土微结构表面起伏的结构。通过改进的射影覆盖法,计算出塌陷前的黄土分形维数为2.508,塌陷后为2.590,表明塌陷后的黄土的微观结构表面起伏程度增加,孔隙复杂度明显增加。

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