4.7 Article

Gradients estimation from random points with volumetric tensor in turbulence

期刊

JOURNAL OF COMPUTATIONAL PHYSICS
卷 350, 期 -, 页码 518-529

出版社

ACADEMIC PRESS INC ELSEVIER SCIENCE
DOI: 10.1016/j.jcp.2017.08.057

关键词

Volumetric tensor; Spatial derivative; Turbulence; Lagrangian simulations

资金

  1. Collaborative Research Project on Computer Science with High-Performance Computing in Nagoya University
  2. MEXT KAKENHI Grant [16K18013]
  3. Grants-in-Aid for Scientific Research [16K18013] Funding Source: KAKEN

向作者/读者索取更多资源

We present an estimation method of fully-resolved/coarse-grained gradients from randomly distributed points in turbulence. The method is based on a linear approximation of spatial gradients expressed with the volumetric tensor, which is a 3 x 3 matrix determined by a geometric distribution of the points. The coarse grained gradient can be considered as a low pass filtered gradient, whose cutoff is estimated with the eigenvalues of the volumetric tensor. The present method, the volumetric tensor approximation, is tested for velocity and passive scalar gradients in incompressible planar jet and mixing layer. Comparison with a finite difference approximation on a Cartesian grid shows that the volumetric tensor approximation computes the coarse grained gradients fairly well at a moderate computational cost under various conditions of spatial distributions of points. We also show that imposing the solenoidal condition improves the accuracy of the present method for solenoidal vectors, such as a velocity vector in incompressible flows, especially when the number of the points is not large. The volumetric tensor approximation with 4 points poorly estimates the gradient because of anisotropic distribution of the points. Increasing the number of points from 4 significantly improves the accuracy. Although the coarse grained gradient changes with the cutoff length, the volumetric tensor approximation yields the coarse grained gradient whose magnitude is close to the one obtained by the finite difference. We also show that the velocity gradient estimated with the present method well captures the turbulence characteristics such as local flow topology, amplification of enstrophy and strain, and energy transfer across scales. (C) 2017 Elsevier Inc. All rights reserved.

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