1971
DOI: 10.1017/s002211207100034x
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A numerical study of the Bénard cell

Abstract: When a layer of liquid is heated from below at a rate which exceeds a certain critical value, a two- or three-dimensional motion is generated. This motion arises from the action of buoyancy and surface tension forces, the latter being due to variations in the temperature of the liquid surface.The two-dimensional form of the flow has been studied by a numerical method. It consists of a series of rolls, rotating alternately clockwise and anticlockwise, which are shown to be symmetrical about the dividing streaml… Show more

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Cited by 11 publications
(6 citation statements)
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References 16 publications
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“…After each half-time increment, an updated estimate was made of the stream function by solving Equation ( 15). A point over-relaxation procedure was used (Smith, 1971) with the over-relaxation parameter being empirically varied in successive solution processes to minimize the required number of iterations (Cabelli, 1970). A relative convergence criterion was used to terminate this stage.…”
Section: St-rt Modelmentioning
confidence: 99%
See 1 more Smart Citation
“…After each half-time increment, an updated estimate was made of the stream function by solving Equation ( 15). A point over-relaxation procedure was used (Smith, 1971) with the over-relaxation parameter being empirically varied in successive solution processes to minimize the required number of iterations (Cabelli, 1970). A relative convergence criterion was used to terminate this stage.…”
Section: St-rt Modelmentioning
confidence: 99%
“…Douglas (1962) showed that when a similar method is used, the overall accuracy improves from first to second order in time. An accelerated rate of convergence and a reduction in computation time of 10 to 15% was obtained by empirically varying the time step after each iteration (Cabelli, 1970).…”
Section: St-rt Modelmentioning
confidence: 99%
“…Among dissipative systems observed, Turing's reaction-diffusion and Rayleigh-Bénard (R-B) convection are the two representative systems for spatial pattern formation, and they have been actively studied because of their analytical and experimental accessibility. [13][14][15][16][17][18][19][20][21][22][23][24][25] Although the appeared structures either in scales or formation process are different for diverse dissipative systems, their morphologies are similar. 26 For example, line patterns, square-grid arrays, zig-zag patterns etc.…”
Section: Introductionmentioning
confidence: 99%
“…Other data not available. Fick's Law apparently valid Very few collapse pressure and collapse rate data available, and these pertain to mono layers at the air-water interface [52 ] Measurements available for a variety of surfactants at the air-water and oil-water [55] interface, but little agreement amongst investigators useful in constructing semi -em pirical models of the developed convection for purposes of predicting heat or mass transfer accompanying interfacial convection [57][58][59][60].…”
Section: Introductionmentioning
confidence: 99%