2015
DOI: 10.1002/num.22043
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Antidiffusive Lagrangian‐remap schemes for models of polydisperse sedimentation

Abstract: One-dimensional models of gravity-driven sedimentation of polydisperse suspensions with particles that belong to N size classes give rise to systems of N strongly coupled, nonlinear first-order conservation laws for the local solids volume fractions. As the eigenvalues and eigenvectors of the flux Jacobian have no closed algebraic form, characteristic-wise numerical schemes for these models become involved. Alternative simple schemes for this model directly utilize the velocity functions and are based on split… Show more

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Cited by 3 publications
(5 citation statements)
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“…We extended the L-AR schemes proposed in [5,6] to the non-local multi-class traffic flow model proposed in [10]. We provided some properties of the L-AR scheme and we proved the convergence to weak solutions in the scalar case.…”
Section: Discussionmentioning
confidence: 99%
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“…We extended the L-AR schemes proposed in [5,6] to the non-local multi-class traffic flow model proposed in [10]. We provided some properties of the L-AR scheme and we proved the convergence to weak solutions in the scalar case.…”
Section: Discussionmentioning
confidence: 99%
“…The aim of this paper is to present a generalization to non-local systems of the Lagrangian-Antidiffusive Remap (L-AR) schemes introduced in [5,6], in order to compute approximate solutions of model (1.1). This type of schemes are constructed exploiting the concentrationtimes-velocity form of the fluxes in (1.1).…”
Section: Introductionmentioning
confidence: 99%
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“…Remark 6.1. In the case S ≡ 0, system (6.1) has the same structure as the classical Keytz-Kranzer system [35] up to the properties of the ux function f which is monotone in the Keytz-Kranzer case and which is bell-shaped in the case we are concerned with, see also [15]. Discretization of the Keytz-Kranzer system by nite dierence schemes was addressed, in particular, in [36].…”
Section: Motivationmentioning
confidence: 99%
“…General references to models of sedimentation include [6,33]. Models of polydisperse sedimentation in one space dimension similar to the MLB model, and which give rise to strongly coupled systems of nonlinear conservation laws or possibly degenerate convection-diffusion equations were thoroughly studied in recent years including analyses of hyperbolicity [13,23], extensions to flocculated suspensions forming compressible sediments [8], construction of entropy solutions [7,24], development of efficient numerical schemes [10,14,15], and applications in geophysics [25], water resource recovery [16], and others (see also references in the cited works). On the other hand, theoretical and experimental works on polydisperse gravity currents, with which our numerical results could in principle be compared, include [9,21,30].…”
Section: Related Workmentioning
confidence: 99%