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Study on Fractal Theory in Identifing Soil Fabric in Civil Engineering

机译:分形理论在土木工程中识别土壤织物的分形理论研究

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Soil fabric describes the arrangement, shape, size, and size distribution of the mineral constituents of a soil. On a small scale, the soil micro-fabric can be studied by looking at undisturbed samples under a scanning electron microscope or it can be described under high-resolution optical microscope in thin section. Different kinds of soil fabrics indicated different sedimentary environments under which the soils formed before; also it could show the information of different property and distinct material composition of soils. Engineering properties of soil were connected tightly with its structure and fabric. In geo-technique science, there existed many methods to describe the soil's structure and fabric. It has been proved that fractal dimension and multi-fractal theory are efficient way in the studying of soil's fabric. With the help of fractal dimension and multi-fractal spectrum, efforts were taken to analyze the micro-porous structural features in great overburden clay. The study shows that fractal dimension can distinguish the fine difference between the two type of soil such as undisturbed soil sample and dry shrinkage soil sample. The multi-fractal spectrum of these two kinds of soil showed the same conclusion.
机译:土壤面料描述了土壤中矿物成分的布置,形状,尺寸和尺寸分布。在小规模上,通过在扫描电子显微镜下观察未受干扰的样品,可以研究土壤微织物,或者可以在薄截面中在高分辨率光学显微镜下描述。不同种类的土壤织物表明了不同沉积环境,在此之前形成的土壤;此外,它也可以显示不同性质和不同的土壤的不同材料组成的信息。土壤的工程性质紧紧地连接其结构和织物。在地质技术科学中,存在许多方法来描述土壤的结构和织物。事实证明,分形维数和多分形理论是在研究土壤织物的有效方法。借助分形维数和多分形光谱,采取努力分析大覆盖粘土中的微孔结构特征。该研究表明,分形尺寸可以区分两种土壤之间的细差,如未受干扰的土壤样品和干燥收缩土壤样品。这两种土壤的多分形光谱显示得出相同的结论。

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