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Modeling of Sediment Particle Deposition and Resuspension Processes Using a Stochastic Jump Diffusion Particle Tracking Model

机译:使用随机跳跃扩散粒子跟踪模型建模沉积物粒子沉积和重悬浮过程

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Although river beds generally tend to reach an asymptotic equilibrium, it may be abruptly altered by occurrences of natural extreme flow events or establishment of man-made structures. These causes lead to significant morphological changes in the bed profile through erosion and deposition processes. The change of river bed can be quantified for predicting the stability of a river channel. The status of a geomorphological equilibrium can be determined by two transport phases, i.e., water and sediment transport. In particular, the bed profile in sediment transport models can be employed as the initial condition, and the calculated movement of sediment can set a new bed profile. Herein, we propose to use the stochastic jump diffusion particle tracking model (SJD-PTM) to simulate the movement of sediment and particle deposition and resuspension processes. The stochastic diffusion jump particle tracking model is a Lagrangian particle tracking model governed by stochastic equations. When simulating the particle trajectories from the mean drift, settling velocity, diffusivity and extreme events, we can calculate the probabilities of deposition/scouring of a sediment particle by comparing the particle shear stress with the critical shear stress. As the result, we can trace particles and obtain particle trajectories and their statistical characteristics such as the ensemble mean and variance. Furthermore, we will be able to simulate particle deposition and resuspension processes.
机译:虽然河床通常往往达到渐近均衡,但是由于自然极端流动事件或建立人造结构,可能会突然改变。这些原因通过腐蚀和沉积过程导致床型材的显着形态变化。可以量化河床的变化,以预测河流通道的稳定性。地貌均衡的状态可以通过两个运输阶段,即水和沉积物传输来确定。特别地,沉积物传输模型中的床轮廓可以用作初始条件,并且沉积物的计算运动可以设定新的荫的轮廓。在此,我们建议使用随机跳跃扩散粒子跟踪模型(SJD-PTM)来模拟沉积物和颗粒沉积和重悬浮过程的运动。随机扩散跳跃粒子跟踪模型是由随机方程控制的拉格朗日粒子跟踪模型。当模拟平均漂移的粒子轨迹,沉降速度,扩散和极端事件时,我们可以通过将颗粒剪切应力与临界剪切应力进行比较来计算沉积物颗粒的沉积/擦除的概率。结果,我们可以追踪粒子并获得粒子轨迹及其统计特征,例如集合均值和方差。此外,我们将能够模拟粒子沉积和重悬浮过程。

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