𝔖 Bobbio Scriptorium
✦   LIBER   ✦

A finite element solution of double diffusive convection

✍ Scribed by V. Dakshina Murty


Publisher
Elsevier Science
Year
1988
Tongue
English
Weight
436 KB
Volume
15
Category
Article
ISSN
0735-1933

No coin nor oath required. For personal study only.

✦ Synopsis


The finite element method is used to analyze double diffusive convection in a rectangular box. The dimensions of the domain are chosen such that it matches exactly with a unit cell. Three cases are studied which correspond to three sets of boundary conditions on the walls. Numerical results are presented for Prandtl numbers from 0.i to I0.0 and thermal Rayleigh number ranging from 2,000 to i0,000. Solute Rayleigh number is held constant at 1,000 throughout the study. The type of element used is the eight noded element with all dependent variables except the pressure interpolated quadratically and the pressure interpolated linearly. Numerical results are presented in terms of isotherms, streamlines, and isohals. Oscillatory solutions are obtained for a certain range of thermal Rayleigh numbers from the steady state algorithm. The oscillations can be seen in terms of the numerical solution oscillating from iteration to iteration about a mean solution.

r ,~V' ~V'~ T' C' ~ 2 z Lu ~.r~ --~ (3) __ v'T~" j-Pa -m * V' v' Pr T S


πŸ“œ SIMILAR VOLUMES


Finite element solutions of convective d
✍ K. E. Barrett; G. Demunshi πŸ“‚ Article πŸ“… 1979 πŸ› John Wiley and Sons 🌐 English βš– 662 KB

Three weighted residual methods are used to analyse several linear and nonlinear model problems related to the stream function-vortidty formulation of the Navier-Stokes equations. These methods are then used to solve the driven cavity problem. 'The results obtained at Reynolds numbers of 100 and 400

Finite element solution of steady natura
✍ Sen, Swarnendu ;Sarkar, A. πŸ“‚ Article πŸ“… 1994 πŸ› John Wiley and Sons 🌐 English βš– 627 KB

## Abstract Use of upwind finite element methods was so far confined to forced convection problems. The present work is devoted to the application of false diffusion techniques to phenomena involving natural convection. A range of Rayleigh numbers in which the discretization by the conventional Gal