首页|开挖卸荷与孔隙水压耦合作用下千枚岩蠕变力学特性研究

开挖卸荷与孔隙水压耦合作用下千枚岩蠕变力学特性研究

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开挖扰动会使矿山岩体受到高应力集中和应力重新分布的影响,而水力因素则会降低岩体强度,研究开挖卸荷与孔隙水压耦合作用下矿山的岩石力学特性,对于确保矿山岩体长期稳定性具有重要意义.选取江西省银山矿边坡岩体作为样本,开展了分级加载蠕变试验,研究了开挖卸荷与孔隙水压耦合作用下千枚岩的蠕变力学特性.结果表明:在相同开挖卸荷条件下,饱和千枚岩的瞬时应变、蠕变应变和稳态蠕变速率均随孔隙水压的增加而增大,瞬时弹性模量和长期强度随孔隙水压的增加而降低;当孔隙水压相同时,受开挖扰动试样的瞬时应变、瞬时弹性模量和长期强度随开挖卸荷程度的增强而降低,蠕变应变和稳态蠕变速率随开挖卸荷程度的增强而增大.
Study on the Creep Mechanical Properties of Phyllite Under the Coupling Effect of Excavation Unloading and Pore Water Pressure
Excavation disturbances induce high stress concentrations and stress redistribution within the mine rock body.Additionally,hydraulic factors diminish the rock body's strength.Mines situated in the southern region of China are particularly susceptible to disasters during the rainy season due to the influence of rainfall.Therefore,investigating the combined effects of these factors on the mechanical properties of mine rock is of significant importance for ensuring the long-term stability of mine side slopes.The study utilized a slope rock body from the Yinshan Mine in Jiangxi Province as a sample and conducted a graded loading creep test based on a triaxial compression test to investigate the mechanical properties of millimeter-scale rock under the combined effects of excavation unloading and pore water pressure.The results indicate that,with increasing excavation unloading and pore water pressure,the short-term peak strength and elastic modulus of the saturated millimeter-scale rock progressively decrease.Under identical excavation unloading conditions,an increase in pore water pressure leads to a reduction in the strength of saturated millimeters due to the influence of the pore water pressure.This results in an increase in transient strain,a decrease in the transient elasticity modulus,and a reduction in resistance to deformation.Additionally,both creep strain and steady-state creep plasticity exhibit exponential growth with the increase in axial stress up to a certain threshold.Under identical pore water pressure conditions,the instantaneous strain and instantaneous elastic modulus of the excavation-disturbed specimen are lower than those of the undisturbed specimen.Additionally,the creep strain and creep rate escalate with the increasing degree of unloading due to excavation.This observation suggests that excavation-induced disturbances diminish the rock strength,rendering the rock body more susceptible to deformation.The findings indicate that the rock strength of phyllite is diminished due to excavation disturbances,rendering the rock mass more susceptible to creep damage.The study further reveals that the combined effects of excavation unloading and pore water pressure exacerbate this reduction in strength.Consequently,the rock mass becomes increasingly prone to creep damage,thereby compromising the stability of slopes.

excavation unloadingpore water pressurephyllitemechanical propertycreep testcoupling effect

蔡鸿宇、王运敏、李小双、耿加波

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江西理工大学应急管理与安全工程学院,江西 赣州 341000

金属矿山安全与健康国家重点实验室,安徽 马鞍山 243000

常州大学城市建设学院,江苏 常州 213164

齐鲁理工学院土木工程学院,山东 济南 250200

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开挖卸荷 孔隙水压 千枚岩 力学特性 蠕变试验 耦合作用

2024

黄金科学技术
中国科学院资源环境科学信息中心

黄金科学技术

CSTPCD北大核心
影响因子:0.651
ISSN:1005-2518
年,卷(期):2024.32(6)