Compact computations based on a stream-function-velocity formulation of two-dimensional steady laminar natural convection in a square cavity
A class of compact second-order finite difference algorithms is proposed for solving steady-state laminar natural convection in a square cavity using the stream-function-velocity (ψ-u) form of Navier-Stokes equations. The stream-function-velocity equation and the energy equation are all solved as a...
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Published in: | Physical review. E, Statistical, nonlinear, and soft matter physics Vol. 85; no. 3 Pt 2; p. 036703 |
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Main Authors: | , |
Format: | Journal Article |
Language: | English |
Published: |
United States
01-03-2012
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Online Access: | Get full text |
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Summary: | A class of compact second-order finite difference algorithms is proposed for solving steady-state laminar natural convection in a square cavity using the stream-function-velocity (ψ-u) form of Navier-Stokes equations. The stream-function-velocity equation and the energy equation are all solved as a coupled system of equations for the four field variables consisting of stream function, two velocities, and temperature. Two strategies are considered for the discretizaton of the temperature equation, which are a second-order five-point compact scheme and a fourth-order nine-point compact scheme, respectively. The numerical capability of the presented algorithm is demonstrated by the application to natural convection in a square enclosure for a wide range of Rayleigh numbers (from 10(3) to 10(8)) and compared with some of the accurate results available in the literature. The presented schemes not only show second-order accurate, but also prove effective. For larger Rayleigh numbers, the algorithm combining the second-order compact scheme for the stream-function-velocity equation with the fourth-order compact scheme for the temperature equation performs more stably and effectively. |
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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 1539-3755 1550-2376 |
DOI: | 10.1103/PhysRevE.85.036703 |