Fractal structure features of granulometric distribution in sliding zone soils of landslides are studied based on the fractal theory.
本文据分形理论分析了滑坡滑动带土粒度分布的分形结构特征。
The SEM test results indicate that the grain size of the material become bigger with the temperature rising but the granulometric distribution has a still uniform distribution.
SEM测试表明材料的粒径随着温度的升高而迅速增大，但颗粒的分布比较均匀。
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