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细粒砂岩在循环加、卸载条件下变形实验
引用本文:许江,王维忠,杨秀贵,王鸿.细粒砂岩在循环加、卸载条件下变形实验[J].重庆大学学报(自然科学版),2004,27(12):60-62.
作者姓名:许江  王维忠  杨秀贵  王鸿
作者单位:重庆大学西南资源开发及环境灾害控制工程教育部重点实验室,重庆大学西南资源开发及环境灾害控制工程教育部重点实验室,重庆大学西南资源开发及环境灾害控制工程教育部重点实验室,重庆大学西南资源开发及环境灾害控制工程教育部重点实验室 重庆 400030,重庆 400030,重庆 400030,重庆 400030
基金项目:教育部春晖计划项目 , 重庆市院士基金 , 教育部优秀青年教师资助计划
摘    要:通过对细粒砂岩在不同位移速率、不同载荷水平时循环加、卸载条件下变形的演化规律的实验研究发现,细粒砂岩在循环加、卸载条件下的卸载曲线与加载曲线不相重合,将形成一封闭的塑性滞回环,且该塑性滞回环从第2次循环起几乎不发生变化.同时还发现,从第2次循环起,每次循环加、卸载完成后所产生的残余位移量也几乎接近于零.另外,对实验结果的综合分析还发现,随着位移速率的增大,载荷-位移曲线的斜率有逐渐增加的趋势,随着载荷水平的提高,第1次循环加、卸载完成后所残余的位移量将有所增加.

关 键 词:循环载荷  变形特性  塑性滞回环  细粒砂岩  细粒砂岩  循环  卸载条件  变形实验  Conditions  Loading  and  Unloading  Characteristics  Deformation  Study  趋势  位移曲线  综合分析  结果  位移量  变化  发生  塑性滞回环  封闭  加载  发现
文章编号:1000-582X(2004)12-0060-03
修稿时间:2004年9月20日

Experimental Study on the Deformation Characteristics of Fine-Sandstone Under the Loading and Unloading Conditions
XU Jiang,WANG Wei-zhong,YANG Xiu-gui,WANG Hongl Disaster Control Engineering Under the State Ministry of Education,Chongqing University,Chongqing,China.Experimental Study on the Deformation Characteristics of Fine-Sandstone Under the Loading and Unloading Conditions[J].Journal of Chongqing University(Natural Science Edition),2004,27(12):60-62.
Authors:XU Jiang  WANG Wei-zhong  YANG Xiu-gui  WANG Hongl Disaster Control Engineering Under the State Ministry of Education  Chongqing University  Chongqing  China
Institution:XU Jiang,WANG Wei-zhong,YANG Xiu-gui,WANG Hongl Disaster Control Engineering Under the State Ministry of Education,Chongqing University,Chongqing 400030,China)
Abstract:The deformation characteristics of the fine-sandstone is studied under the loading and unloading conditions at the three different deformation-rates and the two different stress-levels. The experimental results show that there is really the plastic-loop in the deformation curve for the loading deformation curve is different from the unloading deformation curve. But the plastic-loop is nearly unchangeable since the second circulate loading. The residual-deformation is be almost zero since the second circulate loading, and that the slope of the deformation curve increases as the deformation-rate increases, and that the residual-deformation increases as the stress-levels increases.
Keywords:the loading and unloading conditions  the deformation characteristics  the plastic-loop  fine-sandstone
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