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。
Fractal structure features of granulometric distribution in sliding zone soils of landslides are studied based on the fractal theory.
滑动带土的粒度分维值一般在2～3之间，其平均值约为2．8，分维可作为描述滑动带土粒度成分的参数。
The fractal dimensions of grain size of slipped zone are 2 to 3, and average on about 2.8. The fractal dimension of granulometric composition can bet…
滑动带土的粒度分维值一般在2～3之间，其平均值约为2．8，分维可作为描述滑动带土粒度成分的参数。
The fractal dimensions of grain size of slipped zone are 2 to 3, and average on about 2.8. The fractal dimension of granulometric composition can bet…
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