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个人信息Personal Information
教授
博士生导师
硕士生导师
主要任职:大连理工大学白俄罗斯国立大学联合学院院长、直属党支部书记
其他任职:辽宁省极地海洋专业技术创新中心主任
性别:男
出生日期:1972-12-30
毕业院校:大连理工大学
学位:博士
所在单位:力学与航空航天学院
学科:计算力学. 固体力学. 工程力学. 船舶与海洋结构物设计制造. 岩土与环境力学
办公地点:大连理工大学主校区海宇楼(1号实验楼)607室
联系方式:0411-84708683
电子邮箱:jisy@dlut.edu.cn
颗粒材料剪切流动状态转变的环剪试验研究
点击次数:
发表时间:2022-10-09
发表刊物:力学学报
所属单位:运载工程与力学学部
期号:5
页面范围:1061-1072
ISSN号:0459-1879
摘要:The shear flow behaviors of granular materials exist widely in the natural disasters (such as landslide and debris flow) and the industrial process (such as transportation and pumping of mineralmaterials). Granular materials perform various shear flow states under different volume fractions, shear rates and constraint stresses. The investigation of mechanical characteristics in a shear flow process provides an insight to the mechanism of phase transition of granular materials. In this study, a medium-size annular shear cell was developed to study the shear flow states of granular materials and their transition. The shear stress and the volume dilation rate were measured under various normal stresses and shear rates. The experimental results show that the shear stress and the volume dilation rate increase with increasing shear rate. Both of them increase with the square of shear rate piecewise linearly. The inflection points in the linear relations of the square of shear rate versus the shear stress and the volume dilation rate were obtained at the critical shear rate respectively. With the analysis of effective friction coe?cients under various shear rates and inertia numbers, the phase transition process between the slow flow and the rapid flow was discussed. The phase transition occurs at the critical shear rate. Moreover, the shear flow states of granular materials were measured under various normal stresses. The critical shear rate decreases with increasing normal stress. This indicates that the normal stress can boost the phase transition between the slow flow state and the rapid flow state. In rapid shear flow state, the e ective friction coe cient is independent of the normal stress. The mechanism of phase transition can be well studied with the experiments of shearing granular under various shear rates and normal stresses.
备注:新增回溯数据