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Reynolds-averaged Navier–Stokes equations with explicit data-driven Reynolds stress closure can be ill-conditioned

Published online by Cambridge University Press:  29 April 2019

Jinlong Wu
Affiliation:
Kevin T. Crofton Department of Aerospace and Ocean Engineering, Virginia Tech, Blacksburg, VA 24060, USA
Heng Xiao*
Affiliation:
Kevin T. Crofton Department of Aerospace and Ocean Engineering, Virginia Tech, Blacksburg, VA 24060, USA
Rui Sun
Affiliation:
Kevin T. Crofton Department of Aerospace and Ocean Engineering, Virginia Tech, Blacksburg, VA 24060, USA
Qiqi Wang
Affiliation:
Department of Aeronautics and Astronautics, MIT, Cambridge, MA 02139, USA
*
†Email address for correspondence: hengxiao@vt.edu

Abstract

Reynolds-averaged Navier–Stokes (RANS) simulations with turbulence closure models continue to play important roles in industrial flow simulations. However, the commonly used linear eddy-viscosity models are intrinsically unable to handle flows with non-equilibrium turbulence (e.g. flows with massive separation). Reynolds stress models, on the other hand, are plagued by their lack of robustness. Recent studies in plane channel flows found that even substituting Reynolds stresses with errors below 0.5 % from direct numerical simulation databases into RANS equations leads to velocities with large errors (up to 35 %). While such an observation may have only marginal relevance to traditional Reynolds stress models, it is disturbing for the recently emerging data-driven models that treat the Reynolds stress as an explicit source term in the RANS equations, as it suggests that the RANS equations with such models can be ill-conditioned. So far, a rigorous analysis of the condition of such models is still lacking. As such, in this work we propose a metric based on local condition number function for a priori evaluation of the conditioning of the RANS equations. We further show that the ill-conditioning cannot be explained by the global matrix condition number of the discretized RANS equations. Comprehensive numerical tests are performed on turbulent channel flows at various Reynolds numbers and additionally on two complex flows, i.e. flow over periodic hills, and flow in a square duct. Results suggest that the proposed metric can adequately explain observations in previous studies, i.e. deteriorated model conditioning with increasing Reynolds number and better conditioning of the implicit treatment of the Reynolds stress compared to the explicit treatment. This metric can play critical roles in the future development of data-driven turbulence models by enforcing the conditioning as a requirement on these models.

Information

Type
JFM Papers
Copyright
© 2019 Cambridge University Press 
Figure 0

Table 1.Summary of the results of the channel flow test, showing percentage errors in the turbulent shear stresses and the propagated mean velocities. The large errors in the high-Reynolds-number case $Re_{\unicode[STIX]{x1D70F}}=5200$ are highlighted in bold. The true Reynolds shear stresses are obtained by analytically integrating the RANS equation with the DNS mean velocities (Thompson et al.2016).

Figure 1

Figure 1.Conditioning measure of Reynolds-stress-based turbulence models based on ${\mathcal{K}}_{\unicode[STIX]{x1D63C}}$ and the ratio $\overline{\unicode[STIX]{x1D6FC}}$ as defined in (2.12). The Reynolds stress is computed from DNS data to study the ideal scenario of the RANS modelling.

Figure 2

Figure 2.The balance among forces due to turbulent shear stress ($\unicode[STIX]{x1D735}\boldsymbol{\cdot }\unicode[STIX]{x1D749}$), viscous shear stress ($\unicode[STIX]{x1D735}\boldsymbol{\cdot }\unicode[STIX]{x1D749}_{vis}$) and pressure gradient ($\unicode[STIX]{x1D735}p$) for two plane channel flows at frictional Reynolds numbers (a) $Re_{\unicode[STIX]{x1D70F}}=180$ and (b) $Re_{\unicode[STIX]{x1D70F}}=5200$. The right vertical axis denotes the inner coordinates ($y^{+}$).

Figure 3

Figure 3.Force balance of the plane channel flow in (a) the outer layer and (b) the viscous wall region.

Figure 4

Figure 4.The profiles of local condition number ${\mathcal{K}}_{j}$ at different Reynolds numbers by using explicit treatment with fixed Reynolds stress, i.e. the fixed DNS Reynolds stress is substituted into RANS equations.

Figure 5

Figure 5.The error propagation analysis of solving streamwise velocity iteratively by using explicit treatment with fixed Reynolds stress, including (a) relative error of mean velocity and (b) volume-averaged local condition number.

Figure 6

Figure 6.The local condition number at different Reynolds numbers by using implicit treatment of Reynolds stress, i.e. the linear part of Reynolds stress is implicitly treated by introducing an optimal eddy viscosity.

Figure 7

Figure 7.The volume-averaged local condition number at different Reynolds numbers for explicit and implicit treatments of Reynolds stress.

Figure 8

Figure 8.The error propagation analysis of solving streamwise velocity iteratively by using implicit treatment of Reynolds stress, including (a) relative error of mean velocity and (b) volume-averaged local condition number.

Figure 9

Figure 9.The comparison of solved mean velocity by using explicit and implicit treatments of Reynolds stress, including (a) mean velocity $U$ at $Re_{\unicode[STIX]{x1D70F}}=180$, (b) mean velocity $U$ at $Re_{\unicode[STIX]{x1D70F}}=5200$, (c) percentage error of mean velocity $U$ at $Re_{\unicode[STIX]{x1D70F}}=180$ and (d) percentage error of mean velocity $U$ at $Re_{\unicode[STIX]{x1D70F}}=5200$.

Figure 10

Figure 10.The configuration of (a) the flow in a square duct at $Re_{b}=3500$ and (b) the flow over periodic hills at $Re_{b}=5600$.

Figure 11

Figure 11.The comparison of solved mean velocities by using explicit treatment with fixed Reynolds stress and implicit treatment of Reynolds stress. The computational domain covers a quarter of the cross-section of the physical domain, i.e. $h=D/2$. This is due to the symmetry of the mean flow in both $y$ and $z$ directions as shown in figure 10(a). It should be noted that the Reynolds stress is obtained from a DNS database (Pinelli et al.2010).

Figure 12

Figure 12.The normalized error of the solved secondary flow velocity $U_{z}$ of the flow in a square duct by using (a) explicit treatment with fixed Reynolds stress and (b) implicit treatment of Reynolds stress.

Figure 13

Figure 13.The local condition number of the flow in a square duct by using (a) explicit treatment with fixed Reynolds stress and (b) implicit treatment of Reynolds stress.

Figure 14

Figure 14.The comparison of (a) DNS Reynolds stress and (b) solved mean velocity between different DNS datasets. The solved mean velocity is obtained by substituting the corresponding DNS Reynolds stress and solving RANS equations. The solid black lines in panel (b) denote the DNS mean velocity as a benchmark. It should be noted that the DNS mean velocities from different datasets have no noticeable difference, and here we present the DNS mean velocity from Breuer et al. (2009).

Figure 15

Table 2.Summary of the datasets of the flow over periodic hills at Reynolds number $Re=5600$, including the numerical methods, treatment of solid boundaries, accuracy of numerical discretization, mesh sizes and type. Here $N_{x}$, $N_{y}$, and $N_{z}$ indicate number of grids in streamwise, wall-normal and spanwise directions, respectively.

Figure 16

Figure 15.The local condition number ${\mathcal{K}}_{j}$ of the flow over periodic hills at $Re=5600$ by using (a) explicit treatment with fixed Reynolds stress and (b) implicit treatment of Reynolds stress.

Figure 17

Figure 16.The optimal eddy-viscosity fields for (a) the flow in a square duct at $Re_{b}=3500$ and (b) the flow over periodic hills at $Re_{b}=5600$.

Figure 18

Figure 17.Mesh convergence study of local condition number ${\mathcal{K}}_{j}$ at $Re=5200$ by using explicit treatment with fixed Reynolds stress, i.e. the fixed DNS Reynolds stress is substituted into RANS equations.

Figure 19

Figure 18.The error propagation analysis of solving streamwise velocity iteratively by using explicit treatment of Reynolds stress that depends on the strain rate, including (a) relative error of mean velocity and (b) volume-averaged local condition number.