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基于分形理论的黄土击实后粒度分布研究
引用本文:王效渊,马富丽,白晓红.基于分形理论的黄土击实后粒度分布研究[J].科学技术与工程,2017,17(32).
作者姓名:王效渊  马富丽  白晓红
作者单位:太原理工大学,太原理工大学,太原理工大学
基金项目:国家自然科学基金项目(面上项目,重点项目,重大项目)
摘    要:基于分形理论对不同击实能和含水量条件下的粉土状黄土进行粒度分析,研究击实后土体颗粒形状的变化情况和颗粒体积的分形行为。结果表明,击实后的粉土状黄土颗粒体积分布遵循分形规律;在一定含水量条件下,分维值D会随着击实能的增加而减小;当击实能较大时,对土样颗粒造成的形状改变也更为明显;在一定击实能条件下,当土样含水量小于最优含水量时,分维值D随着含水量的增加而减小;当土样含水量大于最优含水量后,分维值D呈现离散性,没有一定的规律。

关 键 词:分形维数  击实试验  含水量  干密度  击实能
收稿时间:2017/3/29 0:00:00
修稿时间:2017/6/12 0:00:00

Experiment Study on Particle Size Distribution of Compacted Loess Based on Fractal Theory
wangxiaoyuan,and.Experiment Study on Particle Size Distribution of Compacted Loess Based on Fractal Theory[J].Science Technology and Engineering,2017,17(32).
Authors:wangxiaoyuan  and
Institution:Taiyuan University of Technology,,
Abstract:The particle distrubutes of compacted silty loess are studied based on the fractal theory in this paper,study the the change of soil particles and the fractal behavior of particle distrubutes of compacted loess.The results show that particle size of compacted loess follow the fractal pattern,Under the condition of a certain moisture content,fractal dimension D decreases with the increase of compacted energy.When the compacted energy is large,soil particle shape change is more intense.Under the condition of a certain compacted energy,fractal dimension D decreases with the increase of water content when the moisture content is Less than or equal to optimal water content,rendering discreteness when the moisture content is greater than optimal water content.
Keywords:fractal  dimension  compacted  experiment  water  content  dry  density compacted  energy
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