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单轴压缩下横观各向同性岩石破裂过程声发射特性的离散元模拟 被引量:3
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作者 刘京铄 范金星 +1 位作者 李娟 刘斌 《湖南工业大学学报》 2016年第4期5-9,共5页
采用离散单元法研究了横观各向同性岩石在不同层面倾角条件下的单轴压缩破坏过程及声发射特性。结果表明:由于层面倾角的变化,导致横观各向同性岩石破裂过程具有不同的声发射特性。声发射特性与应力存在一定的耦合关系,且声发射空间响... 采用离散单元法研究了横观各向同性岩石在不同层面倾角条件下的单轴压缩破坏过程及声发射特性。结果表明:由于层面倾角的变化,导致横观各向同性岩石破裂过程具有不同的声发射特性。声发射特性与应力存在一定的耦合关系,且声发射空间响应集中在2种岩石的交界面上。互层岩体由于层间力学属性不同,极有可能在交界面处引起应力集中,使得在交界面附近裂纹最先萌生,裂纹进一步向交界面两侧岩体中扩展,从而引起宏观裂纹的出现,最终引起岩体的破坏。随着层面倾角的增大,岩石的单轴抗压强度和弹性模量呈先减小后增大,层面倾角90°时的强度甚至超过了0°时的强度。 展开更多
关键词 横观各向同性岩石 软硬互层 层面倾角 单轴压缩 声发射 离散单元法
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高压水射流冲击作用下横观各向同性岩石破碎机制 被引量:29
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作者 黄飞 卢义玉 +2 位作者 刘小川 敖翔 李良伟 《岩石力学与工程学报》 EI CAS CSCD 北大核心 2014年第7期1329-1335,共7页
基于流体动力学与弹性力学基本理论,分析水射流冲击岩石过程中产生的水锤压力与滞止压力,推导不同压力阶段水射流截面上动压力径向分布函数,建立水射流以不同的夹角α冲击横观各向同性岩石的数学模型,选取α=0°,45°,90°... 基于流体动力学与弹性力学基本理论,分析水射流冲击岩石过程中产生的水锤压力与滞止压力,推导不同压力阶段水射流截面上动压力径向分布函数,建立水射流以不同的夹角α冲击横观各向同性岩石的数学模型,选取α=0°,45°,90°研究冲击夹角对岩石破碎规律的影响;选择具有良好横观各向同性的砂岩开展不同夹角的冲击实验。理论分析与实验研究表明:水锤压力导致横观各向同性岩石产生冲击破碎坑,滞止压力诱发岩石内部裂纹的产生与扩展;水射流以垂直于、倾斜于、平行于层理冲击横观各向同性岩石导致其分别产生横向裂纹、倾斜裂纹和劈裂裂纹。 展开更多
关键词 岩石力学 水射流 冲击荷载 横观各向同性岩石 破碎
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Application of a transversely isotropic brittle rock mass model in roof support design 被引量:1
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作者 David Oliveira 《International Journal of Mining Science and Technology》 SCIE EI 2012年第5期639-643,共5页
Accurate modelling of the potential failure modes in the rock mass is an essential task towards a robust design of roof support systems in coal mines.The use of generalised rock mass properties based on averaged prope... Accurate modelling of the potential failure modes in the rock mass is an essential task towards a robust design of roof support systems in coal mines.The use of generalised rock mass properties based on averaged properties(e.g.Hoek-Brown model) has been found to limit the capability to reproduce the actual rock mass behaviour which may include a wide range of interacting and complex failure mechanisms such as shear and tension fracturing of the intact rock and shear and separation of pre-existing discontinuities,including re-activation.Recent studies have also shown that traditional models,such as the Mohr-Coulomb,may not accurately describe the behaviour of the intact rock,particularly for stress induced failures where spalling and slabbing are observed.This is mainly due to the cohesion and friction components of the shear strength of the intact rock not being mobilised at the same rate with strain-softening of the former component playing an essential role in the post peak behaviour.In addition,coal measure rocks are often transversely isotropic,both by way of the preferred orientation of clay particles within the finer grained lithology and by bedding textures and bedding partings,and this is often ignored in computer simulations.A newly developed transversely isotropic brittle rock mass model is applied in the simulation of a hypothetical and simple roadway development.A Cohesion Weakening-Friction Strengthening(CWFS) approach is adopted to describe the intact rock where the mobilisation and strain-softening of the two shear strength components are linked to plastic deformation.The impacts of anisotropy and brittle rock on the development of the excavation disturbed zone or height of softening,as often referred to,are investigated and their implication in the roof support design discussed. 展开更多
关键词 Transverse isotropy Brittle behaviour Cohesion weakening-friction strengthening Ubiquitous joints
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