摘要
为了揭示黏性土受压时的真实接触面积及细观物理参数的变化规律,利用白光干涉技术测量黏性土在高压应力作用下的真实表面轮廓,对不同压应力作用下表面轮廓点云数据进行分析,并通过Logistic函数推导极限压缩状态下的极限值。结果表明:压缩后的黏性土真实表面轮廓呈偏态分布,存在黏性土颗粒的支撑中心及颗粒压缩接触域;在106~529 MPa的压应力作用下,黏性土实际接触面积占截面面积的比例为0.375~0.431,表观孔隙率为52.5%~55.4%,随着压应力增大,孔隙范围有集中趋势且存在极限值;在支撑中心上、下1倍粒径范围内,表面轮廓分布存在极限渐进值。
To reveal the variation law of real contact area and meso-physical parameters of cohesive soil under compression,white light interference technique was used to measure the real surface profile of cohesive soil under high compressive stress.According to the particle size of cohesive soil,the surface profile point cloud data under different compressive stresses was analyzed,and the limit under limit compression state was derived by using Logistic function.The results show that the real surface profile of the compressed cohesive soil is skewed with the support center of cohesive soil particles and the compression contact area of particles.Under the stress of 106 MPa to 529 MPa,the proportion of real contact area of cohesive soil to cross section area is from 0.375 to 0.431,and the apparent porosity is from 52.5%to 55.4%.As the stress increases,the pore range has a tendency to concentrate and there is a limit.There is a limit asymptotic value on the surface profile distribution within the particle size range of 1 times the support center.
作者
杨苏春
张明义
刘俊伟
管金萍
王永洪
白晓宇
YANG Suchun;ZHANG Mingyi;LIU Junwei;GUAN Jinping;WANG Yonghong;BAI Xiaoyu(School of Civil Engineering,Qingdao University of Technology,Qingdao 266033,Shandong,China)
出处
《济南大学学报(自然科学版)》
CAS
北大核心
2020年第5期490-497,共8页
Journal of University of Jinan(Science and Technology)
基金
国家自然科学基金项目(51778312)
山东省重点研发计划项目(2017GSF16107)。
关键词
白光干涉
黏性土
压应力
孔隙率
接触面积
white light interference
cohesive soil
compressive stress
porosity
contact area