Quantitative test of the time dependent Gintzburg-Landau equation for sheared granular flow in two dimensions

K. Saitoh; Hisao Hayakawa

doi:10.1063/1.4812816

Quantitative test of the time dependent Gintzburg-Landau equation for sheared granular flow in two dimensions

K. Saitoh, Hisao Hayakawa

Faculty of Engineering Technology

Research output: Contribution to journal › Article › Academic › peer-review

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Abstract

We examine the validity of the time-dependent Ginzburg-Landau equation of granular fluids for a plane shear flow under the Lees-Edwardsboundary condition derivedfrom a weakly nonlinear analysis through the comparison with the result of discrete element method.We verify quantitative agreements in the time evolution of the area fraction and the velocityfields, and also find qualitative agreement in the granular temperature.

Original language	English
Pages (from-to)	-
Journal	Physics of fluids
Volume	25
Issue number	7
DOIs	https://doi.org/10.1063/1.4812816 https://doi.org/10.1063/1.4812816
Publication status	Published - 18 Jul 2013

Keywords

METIS-308323
IR-93774

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abstract = "We examine the validity of the time-dependent Ginzburg-Landau equation of granular fluids for a plane shear flow under the Lees-Edwardsboundary condition derivedfrom a weakly nonlinear analysis through the comparison with the result of discrete element method.We verify quantitative agreements in the time evolution of the area fraction and the velocityfields, and also find qualitative agreement in the granular temperature.",

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AB - We examine the validity of the time-dependent Ginzburg-Landau equation of granular fluids for a plane shear flow under the Lees-Edwardsboundary condition derivedfrom a weakly nonlinear analysis through the comparison with the result of discrete element method.We verify quantitative agreements in the time evolution of the area fraction and the velocityfields, and also find qualitative agreement in the granular temperature.

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M3 - Article

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Quantitative test of the time dependent Gintzburg-Landau equation for sheared granular flow in two dimensions

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