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基于Bloch动态均匀化理论的节理岩体等效动力参数及频散效应研究

批准号:
12102315
项目类别:
青年科学基金项目(C类)
资助金额:
30.0 万元
负责人:
孟飞
依托单位:
学科分类:
岩体力学与土力学
结题年份:
2024
批准年份:
2021
项目状态:
已结题
项目参与者:
孟飞

项目摘要

结项摘要

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中文摘要
节理岩体是一种非连续材料,有显著的频散效应,但在大尺度动力问题的计算中常需提取其等效力学参数,并简化为均匀连续介质。本项目综合理论分析、室内试验与数值模拟,提出获取节理岩体等效动力参数的动态均匀化方法并研究其频散效应。根据节理的空间分布,选取合适的代表性体积单元,利用Bloch波理论得到不同频率应力波的相速度,求得节理岩体的等效动力参数及其频散曲线。结合宏观尺度的等效动力参数与细观尺度的代表性体积单元振动模态,阐明节理岩体的频散效应及其机理。基于动态均匀化方法,分析节理的空间分布特征、岩石与节理的力学特性等因素的影响,归纳动荷载作用下岩体质量的评价准则。进行分离式霍普金森杆试验,与理论结果相互验证。在有限元软件中嵌入考虑频散效应的动力本构关系,将动态均匀化方法用于实际工程问题的分析中。研究成果可为我国基础设施建设、地下空间开发、资源开采等提供支撑,具有重要的理论意义和工程价值。
英文摘要
Jointed rock masses are heterogeneous materials with significant dispersion effects. They are usually simplified to uniform continuous medium in large-scale dynamic analysis and represented by several effective mechanical parameters. This project systematically proposes a dynamic homogenization method for obtaining the effective dynamic mechanical parameters of jointed rock masses and investigating their dispersion effects based on theoretical analysis, laboratory tests, and numerical simulation. According to the spatial distribution of joints, Representative Volume Element (REV) is selected. Using Bloch wave theory, the phase velocities of stress waves with different frequencies are obtained. Thereby the effective dynamic mechanical parameters and their dispersion curves are calculated. Combining the macroscopic effective dynamic parameters with the mesoscopic vibration modes of REV, the dispersion effect of jointed rock masses and its mechanism can be investigated. Based on the dynamic homogenization method, influence factors including the spatial distribution of joints and the mechanical properties of rocks and joints are analyzed. The criteria for quality evaluation of rock masses under dynamic actions are further summarized. Employing the Split Hopkinson Pressure Bar instrument, the dynamic homogenization theory can be verified and improved. The dynamic constitutive relationship considering the dispersion effect can be embedded in the finite element analysis software, and via this, the dynamic homogenization method can be used in the analysis of practical engineering projects. The output of this research can support the construction of infrastructures, underground space exploitation, mining projects, etc., and have significant impacts on both theory and practice.
岩体内部广泛存在节理、断层、孔隙等结构,其在动力荷载作用下会显著改变应力波的传播特性。传统岩体力学模型难以精确描述这类复杂介质的动态响应。为此,本项目引入超材料研究中的Bloch波动理论,结合均匀化方法与实验技术,系统性研究节理岩体的等效力学参数及频散效应。项目建立周期性节理岩体的波动方程,计算能带图与频散曲线,分析带隙特性,研究节理材料参数和波传播方向对带隙的影响。针对海洋工程常见的多孔礁灰岩,通过CT扫描构建三维数字岩心模型,提出均匀化方法计算等效弹性张量,量化孔隙分布与力学各向异性。开展节理岩体与多孔礁灰岩的静动力学试验,分析多种因素对岩体动力特性的影响规律。项目工作填补了传统连续介质模型的不足,融合了材料科学与岩土力学,可为工程振动控制与安全评估提供理论支撑。
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