2016Physics of FluidsRequires access

Enstrophy production and dissipation in developing grid-generated turbulence

Yi Zhou, Koji Nagata, Yasuhiko SAKAI, Y. Ito, Toshiyuki Hayase

Open publisher page 21 citations

Abstract

Direct numerical simulations are performed to investigate the spatial evolution of small-scale motions in turbulence behind a single square grid. Some aspects of small-scale motions, which are thought to be universal, are examined at different streamwise locations along the centerline. The behavior of small-scale motions at the end of the simulation region resembles the well-known behavior observed in many types of turbulence (e.g., homogeneous isotropic turbulence, fractal-generated turbulence, and plane jet), whereas in the near grid region, the turbulence exhibits quite different properties. For instance, the alignments between the vortex vector and the eigenvectors are relatively weak in the upstream location. In contrast, at the furthermost downstream location, the alignments are close to the case of homogeneous isotropic turbulence. Also, it is demonstrated that the high enstrophy region may not be indispensable for the appearance of the 2/3 power-law at a streamwise location close to the grid.

About this research paper

What this paper is about

Direct numerical simulations are performed to investigate the spatial evolution of small-scale motions in turbulence behind a single square grid. Some aspects of small-scale motions, which are thought to be universal, are examined at different streamwise locations along the centerline. The behavior of small-scale motions at the end of the simulation region resembles the well-known behavior observed in many types of turbulence (e.g., homogeneous isotropic turbulence, fractal-generated turbulence, and plane jet), whereas in the near grid region, the turbulence exhibits quite different properties. For instance, the alignments between the vortex vector and the eigenvectors are relatively weak in the upstream location. In contrast, at the furthermost downstream location, the alignments are close to the case of homogeneous isotropic turbulence. Also, it is demonstrated that the high enstrophy region may not be indispensable for the appearance of the 2/3 power-law at a streamwise location close to the grid.

Why it matters

OpenAlex reports 21 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

Direct numerical simulations are performed to investigate the spatial evolution of small-scale motions in turbulence behind a single square grid. Some aspects of small-scale motions, which are thought to be universal, are examined at different streamwise locations along the centerline. The behavior of small-scale motions at the end of the simulation region resembles the well-known behavior observed in many types of turbulence (e.g., homogeneous isotropic turbulence, fractal-generated turbulence, and plane jet), whereas in the near grid region, the turbulence exhibits quite different properties. For instance, the alignments between the vortex vector and the eigenvectors are relatively weak in the upstream location. In contrast, at the furthermost downstream location, the alignments are close to the case of homogeneous isotropic turbulence. Also, it is demonstrated that the high enstrophy region may not be indispensable for the appearance of the 2/3 power-law at a streamwise location close to the grid.

Key concepts: Enstrophy, Turbulence, Physics, K-epsilon turbulence model, Isotropy, Dissipation, Vortex, K-omega turbulence model

Related papers

Back to paper searchBrowse research topicsOriginal source
Enstrophy production and dissipation in developing grid-generated turbulence — Research Paper | ScholarLens