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Thermal convection simulation in three dimensions by a modified finite element method

Conference ·
OSTI ID:6125030
In the effort to model the advection and dispersion of pollutants in the planetary boundary layer over complex terrain, a relatively simple computer code was developed for solving the three-dimensional Navier-Stokes equations, or variants thereof. The program, which began as an implementation of the Galerkin Finite Element Methoda (GFEM), now incorporates some of the insights and experiences of the finite difference community and has become an eclectic approach to simulating the motion of fluids governed by these equations. In this study, the computer code was applied to the simulation of a Boussinesq fluid contained in a three-dimensional rectangular box which is heated below and cooled above. The temperature difference between these two isothermal surfaces (parameterized by the Rayleigh number, Ra) determines, to a large extent, the complex spatial and temporal thermoconvection patterns. Problems of this sort have received substantial attention recently due to their relevance to natural convection in solar energy collectors, crystal growth in liquids, radioactive waste storage, and more importantly because studying systems of this sort can provide insight into the onset of phase-chaotic-induced turbulence. Presented in the final section are numerical simulations of the two flow configurations observed experimentally, the three and two-roll cell patterns. These results are, to the best of our knowledge, the first calculations of truly time-dependent three-dimensional confined Benard convection at elevated Rayleigh numbers, and they appear to agree well with experiments.
Research Organization:
Lawrence Livermore National Lab., CA (USA)
DOE Contract Number:
W-7405-ENG-48
OSTI ID:
6125030
Report Number(s):
UCRL-85555; CONF-810935-1; ON: DE81028847
Country of Publication:
United States
Language:
English

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