论文标题

冰波动力学的完全拉格朗日DEM-MPS网状模型

A fully Lagrangian DEM-MPS mesh-free model for ice-wave dynamics

论文作者

Junior, Rubens Augusto Amaro, Mellado-Cusicahua, Andrea, Shakibaeinia, Ahmad, Cheng, Liang-Yee

论文摘要

本文基于混合离散元素方法(DEM)和移动粒子半密码(MPS)无网状技术,开发并评估了一种新型的3D完全拉格朗日(基于粒子)的数值模型,用于对高度动态的冰波相互作用进行建模。 MPS和DEM都属于无网状拉格朗日(粒子)技术。该模型将冰波动力学视为多相连续性二氧化物系统。当MPS在基于拉格朗日粒子的域中求解自由表面流的连续方程时,DEM使用多球赫兹式接触动力学模型来模拟冰的浮动运动和相互作用。混合模型可以预测冰浮游的运动和碰撞以及它们与水,边界和任何障碍的相互作用。考虑到DEM和MP的无网格拉格朗日性质,开发的模型具有预测冰浮雕的自由船只(缺乏内部压力)运动的固有能力,例如,在暴力的自由表面流中滑动,滑动,滚动,碰撞和堆积。已经进行了基于浮动块浮子在干燥和湿床上的大坝破裂流动的小规模且具有挑战性的实验,该实验模仿了理想的果酱释放的特征,以提供有用且全面的质量数据,以验证所提出的模型以及其他数值模型。比较了自由表面轮廓的实验和数值结果以及块的位置。结果表明,该模型可以数值繁殖并预测波丝浮动的复杂三维动态行为的能力。总体而言,这项研究是在完全拉格朗日框架内开发冰波动力学的第一项努力,并且可以扩展其结果以深入了解将来对实际冰波或河流冰动态问题的物理学的理解。

This paper develops and evaluates a novel 3D fully-Lagrangian (particle-based) numerical model, based on the hybrid discrete element method (DEM) and moving particle semi-implicit (MPS) mesh-free techniques, for modeling the highly-dynamic ice-wave interactions. Both MPS and DEM belong to mesh-free Lagrangian (particle) techniques. The model considers ice-wave dynamics as a multiphase continuum-discrete system. While the MPS solves the continuum equations of free-surface flow in a Lagrangian particle-based domain, the DEM uses a multi-sphere Hertzian contact dynamic model to simulate the ice floes motion and interaction. The hybrid model predicts the motion and collision of ice floes as well as their interaction with water, boundaries, and any obstacle in their way. Considering the mesh-free Lagrangian nature of both DEM and MPS, the developed model has an inherent ability to predict the free-drift (absence of internal stress) movements of the ice floes, e.g., sliding, rolling, colliding, and piling-up, in violent free-surface flow. A small-scale and challenging experiment based on dam-break flow over dry and wet beds with floating block floes, which mimics the characteristics of an idealized jam release, has been conducted to provide useful and comprehensive quality data for the validation of the proposed model, as well as other numerical models. Experimental and numerical results of the free-surface profile and the position of the blocks are compared. The results show the ability of the model to numerically reproduce and predict the complex three-dimensional dynamic behavior of wave-ice floes interaction. Overall, this study is a first effort toward developing an ice-wave dynamics within a fully Lagrangian framework, and its results can be extended to bring an in-depth understanding of the physics of the real-scale ice-wave or river ice dynamic problems in the future.

扫码加入交流群

加入微信交流群

微信交流群二维码

扫码加入学术交流群,获取更多资源