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考虑水-力耦合和不同应力路径的砂岩卸荷力学特性试验
引用本文:李均奕,王伟,曹亚军,陈超维,朱其志.考虑水-力耦合和不同应力路径的砂岩卸荷力学特性试验[J].河海大学学报(自然科学版),2023,51(3):135-142.
作者姓名:李均奕  王伟  曹亚军  陈超维  朱其志
作者单位:河海大学岩土力学与堤坝工程教育部重点实验室,江苏 南京210098;河海大学岩土工程科学研究所,江苏 南京210098
基金项目:国家自然科学基金(12072102);中国博士后基金(2021M690047);江苏省六大高峰人才项目;江苏高校“青蓝工程”项目
摘    要:为研究不同渗透压力条件下的岩石卸荷力学特性,选取砂岩为研究对象,开展了不同渗透压力和不同应力路径下的三轴卸荷试验,并与常规三轴试验进行对比,比较了不同应力路径下的岩石强度特性,分析了渗透压力对岩石变形和强度参数的影响。试验结果表明:渗透压力的增大会弱化岩石强度,岩石的峰值强度随渗透压力的增大而降低,而轴向变形随渗透压力增大而增加,渗透压力越大,岩石的压密段特征越明显;针对两种不同的卸荷应力路径,恒轴压卸围压路径条件下,岩石的黏聚力不断降低,内摩擦角不断增加,而加轴压卸围压路径条件下,岩石的黏聚力不断增加,内摩擦角逐渐降低。

关 键 词:岩石力学  三轴卸荷  渗透压力  砂岩  水-力耦合
收稿时间:2022/10/6 0:00:00

Experimental study on unloading mechanical characteristics of sandstone considering water-mechanical coupling and different stress paths
LI Junyi,WANG Wei,CAO Yajun,CHEN Chaowei,ZHU Qizhi.Experimental study on unloading mechanical characteristics of sandstone considering water-mechanical coupling and different stress paths[J].Journal of Hohai University (Natural Sciences ),2023,51(3):135-142.
Authors:LI Junyi  WANG Wei  CAO Yajun  CHEN Chaowei  ZHU Qizhi
Affiliation:Key Laboratory of Ministry of Education for Geomechanics and Embankment Engineering, Hohai University, Nanjing 210098;Jiangsu Research Center for Geomechanical Engineering Technology, Hohai University, Nanjing 210098, China
Abstract:In order to study the unloading mechanical properties of rock under different seepage pressures, this paper selects the sandstone as the research object, conducts triaxial unloading tests under different seepage pressures and different stress paths, and compares the results with conventional triaxial tests. The rock strength characteristics under different stress paths are compared, and the effect of seepage pressure on the rock deformation and strength parameters is further analyzed. The test results show that the increase of seepage pressure will weaken the rock strength, the peak strength of rock decreases with the increase of seepage pressure, and the axial deformation increases with the increase of seepage pressure. Aiming at two different unloading stress paths, under the condition of constant axial pressure and unloading confining pressure, the cohesion of rock keeps decreasing and the internal friction angle increases; under the condition of increasing axial pressure and unloading confining pressure, the cohesion of rock keeps increasing and the internal friction angle decreases.
Keywords:rock mechanics  triaxial unloading  seepage pressure  sandstone  water-mechanical coupling
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