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Analyzing and modeling sub-diffusive transport of bedload along a heterogeneous gravel bed using stochastic and statistical methods

机译:利用随机统计方法分析床载床载叶片叶片的分析与建模

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Bedload transport is one of the main mechanisms for sediment transport in rivers. Bedload transport may exhibit anomalous dispersion behavior during the formation of clusters on the surface of a heterogeneous river bed, which cannot be quantified by the classical Fick's law of diffusion. This study simplifies the complex bedload transport process to a "mass-spring-damper" system, which can describe the cluster formation process based on the observed cluster geometry. The simulation results are consistent with the morphology of clusters extracted from the experimental gravel bed in our flume. The level of spatial heterogeneity of individual clusters is characterized to distinguish the planform morphology of each cluster, based on estimation of the HausdorffBesicovitch dimension of the cluster area. Trapping of sediment particles during bedload transport on a heterogeneous gravel bed is quantified using a random walk approach and the birth-death emigration-immigration Markov process. Sub-diffusive dynamics of bedload transport is also modeled simultaneously using the Langevin equation that defines statistical properties of bedload sediments. Further analysis indicates that the microscopic stochastic Langevin equation relates to a macroscopic deterministic equation according to the continuous time random walk (CTRW) theory.
机译:推移质输移是河流泥沙输移的主要机制之一。推移质输运在非均质河床表面形成团簇的过程中可能表现出异常的分散行为,这无法用经典的菲克扩散定律来量化。本研究将复杂的推移质输运过程简化为一个“质量-弹簧-阻尼器”系统,该系统可以根据观测到的团簇几何形状描述团簇形成过程。模拟结果与水槽中从实验砾石层中提取的团聚体形态一致。根据对集群区域Hausdorfbesicovitch维数的估计,对单个集群的空间异质性水平进行表征,以区分每个集群的平面形态。采用随机游走法和生灭迁移马尔可夫过程对非均质砾石床推移质输运过程中泥沙颗粒的捕获进行了量化。同时,还使用定义推移质沉积物统计特性的朗之万方程对推移质输运的次扩散动力学进行了建模。进一步分析表明,根据连续时间随机游动(CTRW)理论,微观随机朗之万方程与宏观确定性方程有关。

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