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Numerical Heat Transfer, Part A: Applications
An International Journal of Computation and Methodology
Volume 50, 2006 - Issue 2
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Original Articles

Natural Convection in a Cubic Cavity: Implicit Numerical Solution of Two Benchmark Problems

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Pages 99-123 | Received 26 Aug 2005, Accepted 05 Jan 2006, Published online: 23 Sep 2006
 

Abstract

Natural convection of air within a cubic cavity, two opposite walls of which are differentially heated, is simulated numerically for Rayleigh numbers of 103, 104, 105, and 106. For each Rayleigh number, two benchmark problems are examined: all four remaining walls are either adiabatic or perfectly conducting. The conservation equations, written using a vorticity–velocity formulation, are discretized with second-order finite differences on uniform grids containing up to 813 points. The equations are solved at all points simultaneously using Newton's method. Solutions on an 813 nonuniform grid are also presented. Excellent agreement with published computational and experimental data is observed, and new benchmark data are reported for the second problem.

Acknowledgments

The authors gratefully acknowledge the financial support of the National Science Foundation under Grant 0137098.

Notes

a Determined to be the benchmark solution. See text for more detail.

b Solution obtained on 413 grid by combining the 413 and 813 uniform grid solutions via Richardson extrapolation.

c Nonuniform grid obtained by a geometric series; see Section 3.1 for details. All other grids are uniform.

d Grid was too coarse to obtain a converged solution.

a 323 nonuniform grid.

b 813 uniform grid.

c 813 uniform grid for Ra = 103; 61 × 45 × 45 nonuniform grid for Ra = 104; and 91 × 45 × 45 nonuniform grid for Ra = 105.

d Richardson extrapolation using 803 and 1203 uniform grids to get final data on 403 uniform grid.

e 813 uniform grid for Ra = 103 and Ra = 104, and 813 nonuniform grid for Ra = 105 and Ra = 106.

a Determined to be the benchmark solution. See text for more detail.

b Solution obtained on 413 grid by combining the 413 and 813 uniform grid solutions via Richardson extrapolation.

c Nonuniform grid obtained by a geometric series; see Section 3.1 for details. All other grids are uniform.

d Grid was too coarse to obtain a converged solution.

a Experimental data.

b 423 nonuniform grid.

c 294,173 tetrahedral elements.

d 40 × 40 × 20 nonuniform grid.

e 40 × 40 × 20 uniform grid.

f 30 × 30 × 30 and 80 × 80 × 40 nonuniform grids.

g 61 × 61 × 31 nonuniform grid.

h 2,048 nonuniform hexahedral elements.

i 813 uniform grid for Ra = 104, Ra = 4 × 104, and Ra = 105. 813 nonuniform grid for Ra = 106.

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