2012
DOI: 10.1103/physreve.85.016207
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Convection in stable and unstable fronts

Abstract: Density gradients across a reaction front can lead to convective fluid motion. Stable fronts require a heavier fluid on top of a lighter one to generate convective fluid motion. On the other hand, unstable fronts can be stabilized with an opposing density gradient, where the lighter fluid is on top. In this case, we can have a stable flat front without convection or a steady convective front of a given wavelength near the onset of convection. The fronts are described with the Kuramoto-Sivashinsky equation coup… Show more

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Cited by 9 publications
(8 citation statements)
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“…The speed of these branches was previously reported in Ref. 27, however, the scale in Fig. 3 of that reference is off by a factor of ffiffi ffi 2 p , therefore our new calculations should replace the previous results.…”
Section: A Steady Solutionssupporting
confidence: 71%
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“…The speed of these branches was previously reported in Ref. 27, however, the scale in Fig. 3 of that reference is off by a factor of ffiffi ffi 2 p , therefore our new calculations should replace the previous results.…”
Section: A Steady Solutionssupporting
confidence: 71%
“…Assuming that j is non-zero, we introduce time and length scales defined by (3), we solve for each component of the stream function w n in terms of the Fourier coefficient of the front height H n , which leads to the fluid velocity at the front height. 27 Consequently, we arrive to an equation that involves only the front height h, and its Fourier coefficients…”
Section: Equations Of Motionmentioning
confidence: 99%
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