2008
DOI: 10.1016/j.apnum.2007.11.018
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Acceleration of lattice Boltzmann models through state extrapolation: a reaction–diffusion example

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Cited by 5 publications
(5 citation statements)
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“…The focus was on the details of the coupling and how information is exchanged. The use of different ∆x and ∆t values in both regions optimized to local stability properties would be a further development, see [5,9,15,16,23,26,31,33,38] and [6,7,27,32,34,39] for guidelines. Also, we used LBM and PDE models which are equivalent in the macroscopic limit.…”
Section: Discussionmentioning
confidence: 99%
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“…The focus was on the details of the coupling and how information is exchanged. The use of different ∆x and ∆t values in both regions optimized to local stability properties would be a further development, see [5,9,15,16,23,26,31,33,38] and [6,7,27,32,34,39] for guidelines. Also, we used LBM and PDE models which are equivalent in the macroscopic limit.…”
Section: Discussionmentioning
confidence: 99%
“…5.2, the first term in (38) cancels with (24). For practical computations, (37) can be substituted in the remainder of (38) to obtain an expression which is independent of ρ F D (x lbe ). The approximate equation for E(x lbe ) is then given by…”
Section: Error Using Ce-1 Coupling For Non-linear Reaction Termmentioning
confidence: 99%
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“…For a fixed value of k, the extrapolation step size m can be chosen such that an adequate norm of the local error estimate (per step or per unit step) is kept below a specified (relative and/or absolute) tolerance. The outline of a possible strategy for the projective method is given in [14]. There we showed how, next to using traditional local error estimation techniques such as Richardson extrapolation or using methods of different order, the local error can also be estimated by using the theoretical error formulae derived in this paper.…”
Section: Discussionmentioning
confidence: 98%
“…In the last decade, this method has been employed to simulate mass transfer problems as with groundwater flow equation as well as solute transport equation. The diffusion equation governs groundwater flow, while advection-diffusion equation describes the solute transport [2,9,10]. It is worth noting that various lattice configurations have been developed for LBM to solve mass transfer equations, containing D1Q2 and D1Q3 for one dimensional problems, D2Q4, D2D5, and D2Q9 for two dimensional problems, in addition to, D3Q15 and D3Q19 for the three dimensions [3,[11][12][13].…”
Section: Introductionmentioning
confidence: 99%