4.7 Article

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

Journal

COLD REGIONS SCIENCE AND TECHNOLOGY
Volume 186, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.coldregions.2021.103266

Keywords

Mesh-free particle-based methods; DEM; MPS; Ice-wave interaction

Funding

  1. Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) [001]
  2. Natural Sciences and Engineering Research Council of Canada (NSERC)
  3. Canada Research Chair Program
  4. Fonds de recherche du Quebec -Nature et technologies (FRQNT)
  5. Petrobras

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This paper introduces a novel three-dimensional fully Lagrangian numerical model for modeling highly dynamic ice-wave interactions, utilizing a hybrid of discrete element method and moving particle semi-implicit mesh-free techniques. The model considers ice-wave dynamics as a multiphase continuum-discrete system, predicting the motion and collision of ice floes as well as their interactions with water, boundaries, and obstacles. It has the inherent ability to predict the free-drift movements of ice floes, showing promising results in reproducing and predicting complex three-dimensional dynamic behavior in wave-ice floes interactions.
This paper develops and evaluates a novel three-dimensional 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 dynamic within a fully Lagrangian framework (i.e. both flow hydrodynamics and ice dynamics in the Lagrangian particle-based system), 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.

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