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Numerical Simulation of Free-Boundary Problems
A numerical procedure based on the Arbitrary Lagrangian-Eulerian (ALE) description of flow is developed to simulate free surface problems. The conservation equations are rewritten using a referential kinematic description where the grid points move independently of the fluid particles. In all the ap...
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Published in: | International journal of computational fluid dynamics 1996-07, Vol.7 (1-2), p.91-118 |
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Main Authors: | , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | A numerical procedure based on the Arbitrary Lagrangian-Eulerian (ALE) description of flow is developed to simulate free surface problems. The conservation equations are rewritten using a referential kinematic description where the grid points move independently of the fluid particles. In all the applications considered in this work, the fluid domain is bounded below by a rigid impermeable wall and above by a vapor-liquid moving interface. The free surface is taken to be resting on vertical spines and the grid points slide up and down along the vertical spines. The two-dimensional unsteady Navier-Stokes equations are discretized in time using Chorin type Projection scheme and pressure is determined from the Poisson equation. Galerkin Finite Element Method with three node triangular elements has been used for spatial discretization
Hydraulic jump with inlet supercritical Froude number 2.0 is solved. The turbulence is modeled using a two-equation k-ε closure model. The surface roller and small recirculation zone near the foot of the jump are found to influence the turbulence characteristics of the jump significantly. The next application considered is the combined buoyancy-driven and thermocapillary-induced convective flows in crystal growth melts. The influence of various parameters on the flow field and free surface deformation is studied. Lastly, the instabilities in the thin film flows draining down an inclined plane arc studied. The results are compared with the available linear stability and non-linear evolution equation results. The phase transition from supercritical to subcritical is investigated in greater detail. |
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ISSN: | 1061-8562 1029-0257 |
DOI: | 10.1080/10618569608940754 |