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Modulation of the turbulence regeneration cycle by inertial particles in planar Couette flow

Published online by Cambridge University Press:  28 December 2018

G. Wang*
Affiliation:
Department of Civil and Environmental Engineering and Earth Sciences, University of Notre Dame, Notre Dame, IN 46556, USA
D. H. Richter*
Affiliation:
Department of Civil and Environmental Engineering and Earth Sciences, University of Notre Dame, Notre Dame, IN 46556, USA
*
†Email addresses for correspondence: gwang4@nd.edu, David.Richter.26@nd.edu
†Email addresses for correspondence: gwang4@nd.edu, David.Richter.26@nd.edu

Abstract

Two-way coupled direct numerical simulations are used to investigate the effects of inertial particles on self-sustained, turbulent coherent structures (i.e. the so-called regeneration cycle) in plane Couette flow at low Reynolds number just above the onset of transition. Tests show two limiting behaviours with increasing particle inertia, similar to the results from previous linear stability analyses: low-inertia particles trigger the laminar-to-turbulent instability whereas high-inertia particles tend to stabilize turbulence due to the extra dissipation induced by particle–fluid coupling. Furthermore, it is found that the streamwise coupling between phases is the dominant factor in damping of the turbulence and is highly related to the spatial distribution of the particles. The presence of particles in different turbulent coherent structures (large-scale vortices or large-scale streaks) determines the turbulent kinetic energy of particulate phase, which is related to the particle response time scaled by the turnover time of large-scale vortices. By quantitatively investigating the periodic character of the whole regeneration cycle and the phase difference between linked sub-steps, we show that the presence of inertial particles does not alter the periodic nature of the cycle or the relative length of each of the sub-steps. Instead, high-inertia particles greatly weaken the large-scale vortices as well as the streamwise vorticity stretching and lift-up effects, thereby suppressing the fluctuating amplitude of the large-scale streaks. The primary influence of low-inertia particles, however, is to strengthen the large-scale vortices, which fosters the cycle and ultimately reduces the critical Reynolds number.

Information

Type
JFM Papers
Copyright
© 2018 Cambridge University Press 
Figure 0

Figure 1.Sketch of various wall regions and boundary layers in wall units (Jiménez & Pinelli 1999; Pope 2000) and the regeneration cycle sub-steps (Hamilton et al.1995; Waleffe 1997; Schoppa & Hussain 2002) in a domain size called ‘minimal’ unit. In the top-right is the flow field in turbulent PCF in miniunit. Large-scale vortex (LSV) is shown by vector fields and coloured by the streamwise vorticity. Large-scale streak (LSS) is shown by the contour of the streamwise velocity magnitude.

Figure 1

Figure 2.Comparison between current study and published data from Kawahara & Kida (2001) and Wang, Abbas & Climent (2017) in single-phase flow at $Re_{b}=400$: (a) mean velocity profiles; (b) fluctuation velocity RMS in three directions.

Figure 2

Table 1.Parameters of baseline numerical simulations. The Reynolds number $Re_{b}\equiv U_{w}h/\unicode[STIX]{x1D708}$, where $U_{w}$ is half of the relative velocity and $h=L_{y}/2$ is half of the gap between two walls. The friction Reynolds number is $Re_{\unicode[STIX]{x1D70F}}\equiv u_{\unicode[STIX]{x03C4}}h/\unicode[STIX]{x1D708}$ and the particle Stokes relaxation time is $\unicode[STIX]{x03C4}_{p}\equiv \unicode[STIX]{x1D70C}_{p}d^{2}/(18\unicode[STIX]{x1D70C}_{f}\unicode[STIX]{x1D708})$, where $d$ represents the particle diameter. The superscript ‘$+$’ is the dimensionless number based on viscous scale, where $\unicode[STIX]{x1D6FF}_{\unicode[STIX]{x1D708}}$, $u_{\unicode[STIX]{x03C4}}$ and $\unicode[STIX]{x1D708}/u_{\unicode[STIX]{x03C4}}^{2}$ correspond to the viscous length scale, velocity scale and time scale, respectively. FCM (force coupling method) is a low-order multipole expansion for capturing finite-size effects used by Wang et al. (2017).

Figure 3

Figure 3.Effect of inertial particles on the turbulence-to-laminar transition as indicated by the temporal evolution of $C_{f}$. This is demonstrated by gradually decreasing $Re_{b}$, density ratio ($r$) and bulk volumetric concentration ($\overline{\unicode[STIX]{x1D6F7}_{V}}$) starting from a fully turbulent simulation at $Re_{b}=500$. (a) Case 500–80–4, decreasing $Re_{b}=500$ to $Re_{b}=290$; (b) case 500–900–4, decreasing $Re_{b}=500$ to $Re_{b}=400$; (c) fixed $Re_{b}=500$ and increasing density ratio $r=80$ to $r=3000$; (d) fixed $Re_{b}=500$ and two density ratios $r=1800$ and $r=3000$, $\unicode[STIX]{x1D6F7}_{b}$ decreasing from $4\times 10^{-4}$ to $1\times 10^{-4}$.

Figure 4

Figure 4.Turbulence–laminar transition threshold indicated by the temporal evolution of $C_{f}$. A ‘conditional’ test of sensitivity due to inertial particle drag force applied in different spatial regions in case 500–3000–4.

Figure 5

Figure 5.(a,b) Contour of temporal average of streamwise vortex stretching term in one single cross-section ($y,z$ plane) within $50$ time units and isolines of temporal and streamwise average of streamwise vorticity within $50$ time units. (c,d) Contour (logarithmic scale) of temporal and streamwise average of normalized concentration by the bulk value and isolines of temporal and streamwise average of streamwise vorticity within $50$ time units. (a,c) Case 500–500–4; (b,d): case 500–900–4.

Figure 6

Figure 6.(a) Contours of the magnitude of the streamwise flow velocity (colourbar in upper left panel) and instantaneous particle positions projected onto the $(y,z)$ cross-section when the LSS is strongest before breakdown, coloured according to magnitude of particle streamwise velocity (colourbar in upper right panel). The particle size shown in the panels is magnified four times for better visualization. Top-left: case 500–80–4; top-right: case 500–500–4; bottom-left: case 500–900–4; bottom-right: case 500–8000–4 (one-way coupling). (b) Mean volume concentration normalized by the bulk concentration. (c) Mean streamwise velocity scaled by $U_{w}$.

Figure 7

Figure 7.RMS velocity fluctuations in cases with density ratios. (a) Fluid phase in three directions. (b–d) Particulate phase in three directions: (b) streamwise direction fluctuation; (c) wall-normal direction fluctuation; (d) spanwise direction fluctuation. In (b–d), fluid phase in single phase is plotted as a reference.

Figure 8

Figure 8.Modal decomposition of the various sub-steps composing the regeneration cycle as shown in figure 1 and outlined in § 4. Four cases are shown: 500–0–0 (unladen), 500–80 (500–80–4 and 500–80–10 with $St_{turb}=0.056$, turbulence enhancement) and 500–900–4 ($St_{turb}=0.625$, turbulence attenuation). (a) ${\mathcal{M}}(n\unicode[STIX]{x1D6FC},m\unicode[STIX]{x1D6FD})$ as in (4.1) representing turbulent kinetic energy contained in the streaks; (b) ${\mathcal{C}}(0,\unicode[STIX]{x1D6FD})$ as in (4.2) representing for the intensity of the LSV; (c) ${\mathcal{S}}(0,\unicode[STIX]{x1D6FD})$ as in (4.5) representing the vorticity stretching effect to LSV; (d) ${\mathcal{L}}(0,\unicode[STIX]{x1D6FD})$ representing the lift-up effect induced by LSV to enhance LSS as in (4.3). The initial $1200$ time units ($h/U_{w}$) are shown.

Figure 9

Table 2.The average and period of five characteristic terms of the regeneration cycle. The error of the period due to the resolution of the signals is in the range of $\pm 2.5$ time units.

Figure 10

Figure 9.Temporal autocorrelation functions of the five signals shown in figure 8. (a) Single-phase flow, case 500–0–0. Suspension flow: (b) case 500–80–4; (c) case 500–900–4.

Figure 11

Figure 10.Temporal cross-correlation functions of the five signals shown in figure 8. (a) Single-phase flow, case 500–0–0. (b) Suspension flow, case 500–80–4. (c) Suspension flow, case 500–900–4. More than $3000$ time units of phase shifts are calculated but only the range of $-100$ to $100$ time units is shown.

Figure 12

Table 3.Time difference (time units) between connected sub-steps of the regeneration cycle. The error due to the resolution of the signals is in the range of $\pm 2.5$ time units.

Figure 13

Figure 11.Sketch of phase difference between connected sub-steps and the period of the regeneration cycle in minimal unit: (a) case 500–0–0 in comparison with (b) case 500–80–4 and (c) case 500–900–4. (d) Qualitative comparison of the averaged value and the amplitude of the signals with single-phase flow.

Figure 14

Figure 12.(a,b) Stretching term and particle feedback term contributions to equation (4.4) with $(0,\unicode[STIX]{x1D6FD})$ integrated within $20. Dashed line: streamwise vortex stretching term. Solid line: particle feedback term. (c,d) Contour of temporal average of streamwise stretching term in one single cross-section ($y,z$ plane) averaged over 50 time units. Included are isolines of temporal- and streamwise-averaged streamwise vorticity. Dashed line: negative streamwise vorticity. Solid line: positive streamwise vorticity. (e,f) Contour of the temporal average of the particle feedback term in one single cross-section ($y,z$ plane) over 50 time units. Isolines are the same as they are in (c,d). (a,c,e) Case 500–80–4. (b,d,f) Case 500–900–4.

Figure 15

Figure 13.Temporal average intensity of vorticity stretching term in (4.5) of 12 pairs of modes. Comparison between single-phase flow (500–0–0) and suspension flow (500–80–4 and 500–900–4).

Figure 16

Figure 14.Phase shifts between vorticity stretching term (six pairs of modes with fixed $p=1,r=-1$) with the meander streak ${\mathcal{M}}(\unicode[STIX]{x1D6FC},0)$. (a) Single-phase flow (500–0–0). Particle-laden flow: (b) case 500–80–4 and (c) case 500–900–4.