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Effects of helicity on dissipation in homogeneous box turbulence

Published online by Cambridge University Press:  28 September 2018

Moritz Linkmann*
Affiliation:
Fachbereich Physik, Philipps-Universität Marburg, Renthof 6, 35032 Marburg, Germany
*
†Email address for correspondence: moritz.linkmann@physik.uni-marburg.de

Abstract

The dimensionless dissipation coefficient $\unicode[STIX]{x1D6FD}=\unicode[STIX]{x1D700}L/U^{3}$, where $\unicode[STIX]{x1D700}$ is the dissipation rate, $U$ the root-mean-square velocity and $L$ the integral length scale, is an important characteristic of statistically stationary homogeneous turbulence. In studies of $\unicode[STIX]{x1D6FD}$, the external force is typically isotropic and large scale, and its helicity $H_{f}$ either zero or not measured. Here, we study the dependence of $\unicode[STIX]{x1D6FD}$ on $H_{f}$ and find that it decreases $\unicode[STIX]{x1D6FD}$ by up to 10 % for both isotropic forces and shear flows. The numerical finding is supported by static and dynamical upper bound theory. Both show a relative reduction similar to the numerical results. That is, the qualitative and quantitative dependence of $\unicode[STIX]{x1D6FD}$ on the helicity of the force is well captured by upper bound theory. Consequences for the value of the Kolmogorov constant and theoretical aspects of turbulence control and modelling are discussed in connection with the properties of the external force. In particular, the eddy viscosity in large-eddy simulations of homogeneous turbulence should be decreased by at least 10 % in the case of strongly helical forcing.

Information

Type
JFM Papers
Copyright
© 2018 Cambridge University Press 
Figure 0

Table 1. Specifications of the numerical simulations. $N$ denotes the number of grid points in each Cartesian coordinate, $Re$ the Reynolds number with respect to the root-mean-square velocity $U$, the integral scale $L$ and the kinematic viscosity $\unicode[STIX]{x1D708}$, $Re_{\unicode[STIX]{x1D706}}$ the Taylor-scale Reynolds number, $\unicode[STIX]{x1D700}$ the dissipation rate, $\unicode[STIX]{x1D6FD}=\unicode[STIX]{x1D700}L_{f}/U^{3}$ the dimensionless dissipation rate, $\unicode[STIX]{x1D6FD}_{L}=\unicode[STIX]{x1D700}L/U^{3}$ the dimensionless dissipation rate with respect to $L$, $\unicode[STIX]{x1D6FF}_{\unicode[STIX]{x1D6FD}}$ and $\unicode[STIX]{x1D6FF}_{\unicode[STIX]{x1D6FD}_{L}}$ the respective standard errors, $\unicode[STIX]{x1D70C}$ the relative kinetic helicity, $\unicode[STIX]{x1D70C}_{f}$ the relative helicity of the forcing, $\unicode[STIX]{x1D702}$ the Kolmogorov microscale, $k_{max}$ the highest resolved wavenumber, $T=L/U$ the large-eddy turnover time and $t/T$ the steady-state run time in units of $T$. The values given for $\unicode[STIX]{x1D700}$, $U$, $L$ and $\unicode[STIX]{x1D70C}$ are ensemble averages, with the ensemble consisting of snapshots taken at intervals of $T$ in order to obtain statistically independent samples. The identifiers D and S refer to dynamic and static forces, respectively. The two sets of simulations using static forces differ in the dimensionality of the force as indicated by the labels 3D and 1D2C.

Figure 1

Figure 1. Value of $\unicode[STIX]{x1D6FD}$ as a function of $\unicode[STIX]{x1D70C}_{f}$ normalised by its value at $\unicode[STIX]{x1D70C}_{f}=0$ from datasets D2, S3D and S1D2C compared to the analytical predictions in (4.10) and (4.25). (a) $\unicode[STIX]{x1D6FD}=\unicode[STIX]{x1D700}L_{f}/U^{3}$, (b) $\unicode[STIX]{x1D6FD}_{L}=\unicode[STIX]{x1D700}L/U^{3}$, where $L$ is the integral scale.

Figure 2

Figure 2. Value of $\unicode[STIX]{x1D700}$ as a function of $U$ on a logarithmic scale for datasets S1D2C, D2 and S3D. The solid line shows the scaling $\unicode[STIX]{x1D700}\sim U^{3}$, which corresponds to a fixed value of $\unicode[STIX]{x1D6FD}$ and $L_{f}$. The grey shading indicates different values of $\unicode[STIX]{x1D70C}_{f}$. A trend can be observed: for a fixed value of $U$, the dissipation rate decreases with increasing forcing helicity.