摘要
借助分形几何理论，探讨红土在不同处理方法下其颗粒粒度的分维变化特征结果表明：红土的颗粒粒度具有线性分形结构的特点是客观存在的事实，其分维值的大小反映了土中颗粒粒度的分布情况。
Based on the Fractal Geometry, an analysis about the features of grain size of laterite under several conditions is made in this paper by terms of fractal dimension (D) which can describe the features The results denote that a linear fractionated structure of the grain size of laterite exists in log-log plot in which the value of D can be a index of its variations and may affect the features of physical and mechanical features of laterite
关键词
红土
颗粒粒度
分维
laterite, grain size, fractal dimension
