首页|三轴压缩下白云岩力学特性及能量演化规律

三轴压缩下白云岩力学特性及能量演化规律

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研究岩石渐进破坏过程和能量演化规律有助于阐释岩石破坏的内在机理.选取白云岩进行三轴压缩试验,分析特征应力和特征应变能的围压效应,探究不同破裂阶段总吸收能、弹性应变能和耗散能之间的关系,阐明其变化机制.研究表明:①随着围压的增加,各特征应力均呈线性增大.峰值应力对应于白云岩的抗压强度,符合Mohr-Coulomb准则.②特征应变能随围压的增加呈线性增长.起裂应力前弹性应变能逐渐积累;致损应力处耗散能开始加速增长;峰值应力处能量的耗散占据主导地位,极易造成不稳定破坏.③岩爆倾向性指数随围压的降低而显著增大,开挖卸荷后应当布设应力释放孔或进行混凝土支护对岩爆进行调控.
Mechanical Properties and Energy Evolution of Dolomite Under Triaxial Compressions
Exploring the progressive failure of rock samples and the law governing energy evolution helps clarifying the inherent mechanism of rock damage.Triaxial compression tests were conducted on dolomite rock samples to investigate the influence of various factors,such as,confining pressure characteristics,the stress and strain energy.The correlations among the total ab-sorbed energy,the elastic strain energy and the dissipated energy at distinct stages of rupture are analyzed,and the potential mechanisms governing their variations are evaluated.The major findings are as follows:(1)With an increase in the confining pressure,all characteristic stresses exhibit a linear growth.The peak stress corresponds to the compressive strength of dolo-mite rock samples,which adhere to the Mohr-Coulomb criterion.(2)As the confining pressure rises,the strain energy increa-ses linearly.The crack initiation stress illustrates the accumulation of the elastic strain energy;while the energy dissipation at the point of crack damage stress initiates accelerated growth and dominates at the peak stress,rendering it susceptible to an un-stable damage.(3)rock burst potential indices increase significantly as the confining pressure decreases.Following the excava-tion and the unloading,it is recommended to install stress-relief holes or concrete supports for the effective control of the rock burst.

Energy EvolutionProgressive Failure of Rock SamplesCharacteristic StressTriaxial CompressionRock Burst

朱伟豪、董璐、李洪亚、马林建、张思懿

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陆军工程大学爆炸冲击防灾减灾全国重点实验室,南京 210007

能量演化 渐进破坏,特征应力 三轴压缩 岩爆

国家自然科学基金优秀青年基金江苏省自然科学面上项目

52222110BK20211230

2024

土工基础
湖北省土木建筑学会,中国科学院武汉岩土力学研究所,武汉市土木建筑学会

土工基础

影响因子:0.238
ISSN:1004-3152
年,卷(期):2024.38(2)
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