2013
DOI: 10.1063/1.4819146
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Asymptotic flow in the depth of narrow cavity

Abstract: It is shown that the viscous fluid motion in the depth of a narrow cavity is a counterflow moving and periodically varying along the cavity length. The obtained exact solutions of the Stokes equations describe unsteady three-dimensional flows, developing as the distance from the cavity surface increases. The found asymptotic motion is common for a variety of boundary conditions and cavity shapes. Creeping flows between parallel and inclined planes, coaxial cylinders, and concentric cones are particularly addre… Show more

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Cited by 3 publications
(4 citation statements)
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“…Most existing studies on annular channel flows have been performed numerically or experimentally [13,[15][16][17], quite often with the aim of investigating the impact of physicochemical contamination along the upper liquid surface. To our knowledge, except for the recent analytical modeling performed by Shtern [18,19] for an annular cavity considered as semi-infinite along the vertical direction, all existing analytical studies devoted to this configuration only focus on the azimuthal flow either when the liquid surface is free of contamination [20] or when it is contaminated [21,22],…”
Section: Introductionmentioning
confidence: 99%
“…Most existing studies on annular channel flows have been performed numerically or experimentally [13,[15][16][17], quite often with the aim of investigating the impact of physicochemical contamination along the upper liquid surface. To our knowledge, except for the recent analytical modeling performed by Shtern [18,19] for an annular cavity considered as semi-infinite along the vertical direction, all existing analytical studies devoted to this configuration only focus on the azimuthal flow either when the liquid surface is free of contamination [20] or when it is contaminated [21,22],…”
Section: Introductionmentioning
confidence: 99%
“…It is interesting that the entire problem formally is nonlinear despite the motion is creeping, but can be reduced to the two linear problems: one for the swirl velocity (5) and the other for the meridional motion (6)- (8). After solving problem (5), the "source" term, v 2 /r in equation (7), is prescribed, so the problem for the meridional motion also is linear.…”
Section: Reduced Problemmentioning
confidence: 99%
“…The number of variables involved in the problem is reduced by introducing a streamfunction-vorticity-circulation form. System (1)-(4) is transformed into three equations for the 8 Stokes stream function Ψ, u = − r −1 ∂Ψ/∂z, w = r −1 ∂Ψ/∂r, the azimuthal vorticity component, η = ∂u/∂z-∂w/∂r, and circulation, Γ = rv:…”
Section: Transformation Of Equationsmentioning
confidence: 99%
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