2008
DOI: 10.4310/cms.2008.v6.n1.a2
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Shallow water viscous flows for arbitrary topopgraphy

Abstract: Abstract. In this paper, we obtain new models for gravity driven shallow water laminar flows in several space dimensions over a general topography. These models are derived from the incompressible Navier Stokes equations with no-slip condition at the bottom and include capillary effects. No particular assumption is made on the size of the viscosity and on the variations of the slope. The equations are written for an arbitrary parametrization of the bottom and an explicit formulation is given in the orthogonal … Show more

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Cited by 26 publications
(30 citation statements)
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“…The latter is a simplified form drawn from a family of models derived by Boutonet, Chupin, Noble, and Vila [2] where we omit, in particular, surface tension and some high-order terms. The present steady shallowwater model is one-dimensional (primes denote derivatives with respect to x 1 ) and expresses conservation of mass and momentum in the form…”
Section: Comparison With a Shallow-water Modelmentioning
confidence: 99%
See 1 more Smart Citation
“…The latter is a simplified form drawn from a family of models derived by Boutonet, Chupin, Noble, and Vila [2] where we omit, in particular, surface tension and some high-order terms. The present steady shallowwater model is one-dimensional (primes denote derivatives with respect to x 1 ) and expresses conservation of mass and momentum in the form…”
Section: Comparison With a Shallow-water Modelmentioning
confidence: 99%
“…Important results in this direction have been achieved by Wierschem,2 Aksel, and Scholle [13,14] using an analytical approach, similar in spirit to that of Yih [15] for a flat plane, based on an expansion of the free-surface Navier-Stokes equations in which the wavelength parameter (essentially the ratio of the film thickness to the wavelength of the bottom undulations) serves as the perturbation parameter. The main result is that the critical Reynolds number for the onset of surface waves is higher than that for a flat bottom.…”
Section: Introductionmentioning
confidence: 99%
“…Find the velocity field u and the mass density field ρ such that conditions (3), (6), (10) and (11) hold.…”
Section: Statement Of the 3d Problemmentioning
confidence: 99%
“…More general constitutive relations may be studied such as those included in [13]. Remark also that depending on the basal boundary condition (slip boundary condition or non-slip boundary condition), various shallow water type equations may be obtained, see for instance [20] and [10] for models coming from incompressible Navier-Stokes equations and [18] for models coming from Bingham type equations with Dirichlet boundary condition at the bottom. Here, we consider boundary conditions in the spirit of [20], namely Navier boundary conditions at the bottom.…”
Section: Introductionmentioning
confidence: 99%
“…We derive thin film models generalizing results by Gerbeau, Perthame, see [15] and F.Marche, see [28] which consider Newtonian fluids with slip boundary condition at the bottom and appropriate range of adimensionnalized numbers. It could be interesting to perform similar asymptotic in Vila's framework, see [7,11] namely with no-slip boundary condition and infinitely large Reynolds number in the limit of infinitely thin layers. See [14] for such generalization but in the Bingham framework.…”
Section: Introductionmentioning
confidence: 99%