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Computational homogenization for mechanical properties of sand cobble stratum based on fractal theory

机译:基于分形理论的砂鹅卵石力学力学性能计算均质化

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AbstractSandy cobble strata is one of the most commonly encountered engineering geological body. A further research into the stability of ground and underground structure demands for precise modeling of actual formation. In this paper, a meso-scale numerical method for modelling sandy cobble strata is presented, which considers rock blocks and soil matrix as separate constituents. In the approach, the particle size distribution and spatial distribution of rock blocks are two crucial points. For the first point, i.e. the particle size distribution of rocks, the fractal scaling theory is included in particle size distribution description and design. In the log-log plots, 60 sets of particle size distributions of sandy cobble soil in Beijing are examined for fractal behavior. For the second point, i.e. the spatial distribution of rocks, the Monte-Carlo principle is used to generate random spatial distribution of rocks in soil matrix, while the rock shape is assumed to be circular in two dimension, or sphere in three dimension. Based on the compassion of rock volume content between the numerical model and theoretical calculation value, it is validated that the meso-scale method could basically be used to establish the meso model of sandy cobble strata. Then, the present sandy cobble strata model is extended to investigate tunnel excavation in such a formation. Based on the simulation results, the deformation characteristics on transverse section and longitudinal profile are explored respectively, and their variations with fractal dimension or the maximum rock size are discussed subsequently.Highlights?A meso-scale numerical method for modelling sand cobble stratum is proposed.?The granularity fractal dimension of sand cobble soil in Beijing ranges from 2.40 to 2.60.?The meso-scale model is extended to investigate the deformation behavior during tunneling.]]>
机译:<![cdata [ 抽象 Sandy Cobble Straata是最常见的工程地质体之一。进一步研究了地面和地下结构的稳定性要求实际地层精确建模。本文提出了一种模拟砂岩层的间谍标准数值方法,其认为岩块和土壤基质作为单独的成分。在该方法中,岩石块的粒度分布和空间分布是两个关键点。对于第一点,即岩石的粒度分布,分形缩放理论包括在粒度分布描述和设计中。在日志记录图中,检查北京的砂岩土壤60套粒度分布以进行分形行为。对于第二点,即岩石的空间分布,Monte-Carlo原理用于在土基质中产生岩石的随机空间分布,而岩石形状被认为是两个尺寸的圆形,或三维球体。基于数值模型和理论计算值之间的岩石体积含量的同情,验证了中间级方法基本可用于建立桑迪鹅卵石地层的中间模型。然后,延长目前的砂皮层模型以调查这种形成的隧道挖掘。基于仿真结果,分别探索横截面和纵向轮廓的变形特性,随后讨论了分形尺寸或最大岩石尺寸的变化。 亮点 提出了一种模拟砂鹅层的中间级数值方法。 < / ce:list-item> 粒度分形维数北京的沙子土壤范围从2.40到2.60。 扩展了Meso-Scale模型以研究隧道期间的变形行为。 ]]>

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