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A level set characteristic Galerkin finite element method for free surface flows
Author(s) -
Lin ChingLong,
Lee Haegyun,
Lee Taehun,
Weber Larry J.
Publication year - 2005
Publication title -
international journal for numerical methods in fluids
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.938
H-Index - 112
eISSN - 1097-0363
pISSN - 0271-2091
DOI - 10.1002/fld.1006
Subject(s) - finite element method , galerkin method , level set method , level set (data structures) , mathematics , free surface , set (abstract data type) , surface (topology) , computational fluid dynamics , discontinuous galerkin method , mathematical analysis , geometry , mechanics , computer science , physics , engineering , structural engineering , artificial intelligence , segmentation , image segmentation , programming language
This paper presents a numerical method for free surface flows that couples the incompressible Navier–Stokes equations with the level set method in the finite element framework. The implicit characteristic‐Galerkin approximation together with the fractional four‐step algorithm is employed to discretize the governing equations. The schemes for solving the level set evolution and reinitialization equations are verified with several benchmark cases, including stationary circle, rotation of a slotted disk and stretching of a circular fluid element. The results are compared with those calculated from the level set finite volume method of Yue et al. ( Int. J. Numer. Methods Fluids 2003; 42 :853–884), which employed the third‐order essentially non‐oscillatory (ENO) schemes for advection of the level set function in a generalized curvilinear coordinate system. The comparison indicates that the characteristic Galerkin approximation of the level set equations yields more accurate solutions. The second‐order accuracy of the Navier–Stokes solver is confirmed by simulation of decay vortex. The coupled system of the Navier–Stokes and level set equations then is validated by solitary wave and broken dam problems. The simulation results are in excellent agreement with experimental data. Copyright © 2005 John Wiley & Sons, Ltd.