2019
DOI: 10.1016/j.jcp.2019.03.034
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Multi-particle model of coarse-grained scalar dissipation rate with volumetric tensor in turbulence

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Cited by 8 publications
(14 citation statements)
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References 63 publications
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“…Numerical schemes except for the filter are the same as those used in the DNS. This LES code was also used for implicit LES of turbulent planar jets and turbulent boundary layers with a passive scalar transfer, where the code was validated by comparison with DNS and experiments (Tanaka, Watanabe & Nagata 2019; Watanabe et al. 2019 b ).…”
Section: Implicit Les and Dns Of A Stably Stratified Shear Layermentioning
confidence: 99%
“…Numerical schemes except for the filter are the same as those used in the DNS. This LES code was also used for implicit LES of turbulent planar jets and turbulent boundary layers with a passive scalar transfer, where the code was validated by comparison with DNS and experiments (Tanaka, Watanabe & Nagata 2019; Watanabe et al. 2019 b ).…”
Section: Implicit Les and Dns Of A Stably Stratified Shear Layermentioning
confidence: 99%
“…. 20 This model is developed on the basis of the estimation for coarse-grained gradients with a volumetric tensor 33 and an SGS model for filtered scalar dissipation rate, which was originally developed for LES of scalar mixing. 19 The model relies on the shape of an energy spectrum of scalar fluctuations and is referred to as a scalar spectrum model.…”
Section: A Scalar Spectrum Model For Coarse-grained Scalar Dissipatio...mentioning
confidence: 99%
“…18,19 One of the SGS models was reformulated for the MVM to model the coarse-grained scalar dissipation rate in LPS. 20 Previous studies have shown that LES/LPS with the MVM can accurately model molecular diffusion in incompressible turbulence. 5,21 There are several variants of the MVM with differences in the number of particles to model the molecular diffusion or in the detailed relaxation process to the average.…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation
“…1998) are applied for spatial discretization, where the accuracy is fourth order in the and directions, and second order in the direction. The third-order Runge–Kutta method is used for temporal advancement, while the biconjugate gradient stabilized (Bi-CGSTAB) method (Van der Vorst 1992) is used to solve the Poisson equation for pressure. An early time period of the flow is simulated by using an implicit large eddy simulation (ILES) like the one conducted in our previous study (Tanaka, Watanabe & Nagata 2019), where the effects of subgrid scales are modelled implicitly by a tenth-order low-pass filter presented in Kennedy & Carpenter (1994), while other numerical schemes are the same as in the DNS. After the TBL fully develops in the ILES, the ILES results are used to initialize the DNS.…”
Section: Tablementioning
confidence: 99%