D

Direct numerical simulation

Simulation in computational fluid dynamics

A direct numerical simulation (DNS) is a simulation in computational fluid dynamics (CFD) in which the Navier–Stokes equations are numerically solved without any turbulence model. This means that the whole range of spatial and temporal scales of the turbulence must be resolved.

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Direct numerical simulation

Simulation in computational fluid dynamics

Texto em inglês

A direct numerical simulation (DNS) is a simulation in computational fluid dynamics (CFD) in which the Navier–Stokes equations are numerically solved without any turbulence model. This means that the whole range of spatial and temporal scales of the turbulence must be resolved.

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Texto em inglês Ainda não há artigo no seu idioma: trecho em inglês.

A direct numerical simulation (DNS) is a simulation in computational fluid dynamics (CFD) in which the Navier–Stokes equations are numerically solved without any turbulence model. This means that the whole range of spatial and temporal scales of the turbulence must be resolved. All the spatial scales of the turbulence must be resolved in the computational mesh, from the smallest dissipative scales (Kolmogorov microscales), up to the integral scale L {\displaystyle L} , associated with the motions containing most of the kinetic energy. The Kolmogorov scale, η {\displaystyle \eta } , is given by η = ( ν 3 / ε ) 1 / 4 {\displaystyle \eta =(\nu ^{3}/\varepsilon )^{1/4}} where ν {\displaystyle \nu } is the kinematic viscosity and ε {\displaystyle \varepsilon } is the rate of kinetic energy dissipation. On the other hand, the integral scale depends usually on the spatial scale of the boundary conditions. To satisfy these resolution requirements, the number of points N {\displaystyle N} along a given mesh direction with increments h {\displaystyle h} , must be N h > L , {\displaystyle Nh>L,\,} so that the integral scale is contained within the computational domain, and also h ≤ η , {\displaystyle h\leq \eta ,\,} so that the Kolmogorov scale can be resolved. Since ε ≈ u ′ 3 / L , {\displaystyle \varepsilon \approx {u'}^{3}/L,} where u ′ {\displaystyle u'} is the root mean square (RMS) of the velocity, the previous relations imply that a three-dimensional DNS requires a number of mesh points N 3 {\displaystyle N^{3}} satisfying N 3 ≥ R e 9 / 4 = R e 2.25 {\displaystyle N^{3}\geq \mathrm {Re} ^{9/4}=\mathrm {Re} ^{2.25}} where R e {\displaystyle \mathrm {Re} } is the turbulent Reynolds number: R e = u ′ L ν . {\displaystyle \mathrm {Re} ={\frac {u'L}{\nu }}.} Hence,...

Texto: Wikipédia em inglês, CC BY-SA 4.0. ·

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