Hostname: page-component-6898cfcb55-w5hgh Total loading time: 0 Render date: 2026-11-11T09:09:34.880Z Has data issue: false hasContentIssue false

Flow dynamics and enhanced mixing in a converging–diverging channel

Published online by Cambridge University Press:  18 October 2016

S. W. Gepner*
Affiliation:
Warsaw University of Technology, Institute of Aeronautics and Applied Mechanics, Nowowiejska 24, 00-665 Warsaw, Poland
J. M. Floryan
Affiliation:
Department of Mechanical and Materials Engineering, The University of Western Ontario, London, Ontario, N6A 5B9, Canada
*
†Email address for correspondence: sgepner@meil.pw.edu.pl

Abstract

An analysis of flows in converging–diverging channels has been carried out with the primary goal of identifying geometries which result in increased mixing. The model geometry consists of a channel whose walls are fitted with spanwise grooves of moderate amplitudes (up to 10 % of the mean channel opening) and of sinusoidal shape. The groove systems on each wall are shifted by half of a wavelength with respect to each other, resulting in the formation of a converging–diverging conduit. The analysis is carried out up to Reynolds numbers resulting in the formation of secondary states. The first part of the analysis is based on a two-dimensional model and demonstrates that increasing the corrugation wavelength results in the appearance of an unsteady separation whose onset correlates with the onset of the travelling wave instability. The second part of the analysis is based on a three-dimensional model and demonstrates that the flow dynamics is dominated by the centrifugal instability over a large range of geometric parameters, resulting in the formation of streamwise vortices. It is shown that the onset of the vortices may lead to the elimination of the unsteady separation. The critical Reynolds number for the vortex onset initially decreases as the corrugation amplitude increases but an excessive increase leads to the stream lift up, reduction of the centrifugal forces and flow stabilization. The flow dynamics under such conditions is again dominated by the travelling wave instability. Conditions leading to the formation of streamwise vortices without interference from the travelling wave instability have been identified. The structure and the mixing properties of the saturated states are discussed.

Information

Type
Papers
Copyright
© 2016 Cambridge University Press 
Figure 0

Figure 1.Channel geometry.

Figure 1

Figure 2.Streamlines of the stationary ($S=0.125$, $\unicode[STIX]{x1D6EF}=5.48\times 10^{-6}$) (a) and a snapshot of an oscillatory ($S=0.150$, $\unicode[STIX]{x1D6EF}=1.15\times 10^{-1}$) (b) velocity field. $\unicode[STIX]{x1D6FC}=1$, $Re=1500$. Computational boxes containing one corrugation wavelength have been used to produce these results.

Figure 2

Figure 3.Development of the recirculation zone for $\unicode[STIX]{x1D6FC}=3$, $Re=2300$, at different corrugation amplitudes: (a) $S=0.075$, (b) $S=0.150$, (c) $S=0.2$ and (d) $S=0.225$ (a snapshot of an oscillatory solution). Computational boxes containing one corrugation wavelength have been used to produce these results.

Figure 3

Figure 4.Variations of the size of the separation zone measured at the widest channel opening as a function of $Re$ for stationary flows. $S=0.025$, $S=0.05$, $S=0.075$, $S=0.1$, $S=0.125$, $S=0.15$, $S=0.175$, $S=0.2$. Computational boxes containing one corrugation wavelength have been used to produce these results.

Figure 4

Figure 5.Variations of the flow rate $Q$ as a function of $Re$ for stationary flows. $S=0.025$, $S=0.05$, $S=0.075$, $S=0.1$, $S=0.125$, $S=0.15$, $S=0.175$, $S=0.2$. Computational boxes containing one corrugation wavelength have been used to produce these results.

Figure 5

Figure 6.Variation of the flow rate $Q$ as a function of the corrugation wavenumber $\unicode[STIX]{x1D6FC}$ for stationary flows. Thick lines identify limits for $\unicode[STIX]{x1D6FC}\rightarrow 0$. Computational boxes containing one corrugation wavelength have been used to produce these results.

Figure 6

Figure 7.Variations of the flow rate based Reynolds number $Re_{av}$ as a function of $Re$ for stationary flows. $S=0.025$, $S=0.05$, $S=0.075$, $S=0.1$, $S=0.125$, $S=0.15$, $S=0.175$, $S=0.2$. The dashed line corresponds to the smooth channel where $Re_{av}=6/4Re$. Computational boxes containing one corrugation wavelength have been used to produce these results.

Figure 7

Figure 8.Variations of the symmetricity parameter (see (2.20) for definition) as a function of $Re$. Flows with $\unicode[STIX]{x1D6EF}>10^{-3}$ are considered to be non-stationary. Internal boxes display instantaneous pressure fields at the jump points. Computational boxes containing one corrugation wavelength have been used to produce these results.

Figure 8

Figure 9.Borders between the stationary and oscillatory states in the $(Re,S)$-plane identified using $\unicode[STIX]{x1D6EF}=10^{-3}$ criterion. Locations of the borders have been determined approximately due to the subcritical character of transition between both states. The intersection of curves for $\unicode[STIX]{x1D6FC}=1$ and $\unicode[STIX]{x1D6FC}=2$ results from the change of the wavenumber $\unicode[STIX]{x1D6FF}$ of the most unstable wave as a function of the amplitude $S$. Computational boxes containing one corrugation wavelength have been used to produce these results.

Figure 9

Figure 10.Variations of the flow rate $Q$ as a function of $Re$ for $\unicode[STIX]{x1D6FC}=1$ and $S=0.2$.$\unicode[STIX]{x1D6EF}=10^{-3}$ criterion has been used to distinguish between the stationary and oscillatory states. Computational boxes containing one corrugation wavelength have been used to produce these results.

Figure 10

Figure 11.Variations of the critical Reynolds numbers $Re_{c}$ of the two most unstable, two-dimensional travelling waves (a) and the corresponding critical frequencies $\unicode[STIX]{x1D70E}_{r,c}$ (b) as functions of the groove amplitude $S$ for $\unicode[STIX]{x1D6FC}=1$. Computational boxes containing one corrugation wavelength have been used to produce these results. $\unicode[STIX]{x1D6FF}=\unicode[STIX]{x1D6FF}_{cr}$ indicates the critical Reynolds number calculated using the immersed boundary conditions (IBC) method (Floryan & Floryan 2010) which permits a nearly continuous variations of $\unicode[STIX]{x1D6FF}$.

Figure 11

Figure 12.Variations of the amplification rate $\unicode[STIX]{x1D70E}_{i}$ (a), and the frequency $\unicode[STIX]{x1D70E}_{r}$ (b) of the travelling wave instability for $\unicode[STIX]{x1D6FC}=1$ for the two most unstable two-dimensional waves as functions of the groove amplitude $S$ for $Re=1000$. Computational boxes containing one corrugation wavelength have been used to produce these results.

Figure 12

Figure 13.Variations of the critical conditions for the two most unstable, two-dimensional waves as functions of the groove amplitude $S$: (a–c) display the critical Reynolds numbers $Re_{c}$ for the groove wavenumbers $\unicode[STIX]{x1D6FC}=0.5,5,8$, respectively, and (d–f) display the corresponding critical frequencies $\unicode[STIX]{x1D70E}_{r,c}$. Computational boxes of length $2\unicode[STIX]{x03C0}$ have been used to produce these results.

Figure 13

Figure 14.Variations of the critical Reynolds number $Re_{c}$ (a) and the critical frequency $\unicode[STIX]{x1D70E}_{r,c}$ (b) for the least stable two-dimensional travelling waves for the corrugation wavenumber $\unicode[STIX]{x1D6FC}=3$ as functions of the corrugation amplitude $S$. Computational boxes with the properly selected lengths have been used to study waves with fractional $\unicode[STIX]{x1D6FF}$ values.

Figure 14

Table 1.Variations of the critical Reynolds number $Re_{cr}$ for oblique travelling waves with the wave vector ($\unicode[STIX]{x1D6FF}=1,2$, $\unicode[STIX]{x1D707}$) as a function of the wave inclination angle expressed in terms of the spanwise wavenumber $\unicode[STIX]{x1D707}$ for grooves with $\unicode[STIX]{x1D6FC}=1$.

Figure 15

Figure 15.Evolution of the kinetic energy of the first Fourier mode (see (3.3)) for flows with $Re=500$ and $Re=2500$ in a channel with $\unicode[STIX]{x1D6FC}=3$, $S=0.05$, $\unicode[STIX]{x1D707}=3.5$. Solid lines illustrate the complete time history while the thick lines identify the data segments used for determination of $A_{k}$ and $B_{k}$ (see (3.4)). Computational box containing one corrugation wavelength has been used to produce these results.

Figure 16

Figure 16.Variations of the vortex amplification rate as a function of the vortex wavenumber $\unicode[STIX]{x1D707}$ for different corrugation wavelengths for $Re=1300$ and $S=0.1$. Computational boxes containing one corrugation wavelength have been used to produce these results.

Figure 17

Figure 17.The neutral stability curves in the $(Re,\unicode[STIX]{x1D707})$-plane for different groove amplitudes $S$. Solid lines correspond to the critical Reynolds numbers for the vortex instability. Dashed lines correspond to the critical Reynolds numbers for the travelling wave instability. ○ Identifies the two-dimensional wave for $S=0.02$ and ▫ identifies such wave for $S=0.2$. Computational boxes containing one corrugation wavelength have been used to produce these results.

Figure 18

Figure 18.Variations of the vortex amplification rate at $\unicode[STIX]{x1D707}_{cr}$ as a function of the groove amplitude and the flow Reynolds number. Computational boxes containing one corrugation wavelength have been used to produce these results.

Figure 19

Figure 19.Variations of the critical Reynolds number $Re_{cr}$ as a function of the groove amplitude $S$. Symbols identify the computed data points. Dotted lines result from the data extrapolation. Computational boxes containing one corrugation wavelength have been used to produce these results.

Figure 20

Figure 20.Variations of the minimum critical Reynolds number $Re_{cr,min}$, the corresponding critical corrugation amplitude $S_{cr}$ and the corresponding reduction of the flow rate as function of the corrugation wavenumber $\unicode[STIX]{x1D6FC}$. Computational boxes containing one corrugation wavelength have been used to produce these results.

Figure 21

Figure 21.Variations of the critical Reynolds number $Re_{cr}$ for the onset of the vortex instability (marked with ) and the two-dimensional travelling wave instability (marked with ) with various wavenumbers $\unicode[STIX]{x1D6FF}$ as a function of the groove amplitude $S$. Thick solid line without any markers in the insert in (b) has been obtained using IBC method. Data for the vortex instability have been determined using computational boxes containing a single corrugation wavelength. Data for the travelling wave instability have been determined using computational boxes containing different number of corrugation wavelengths; boxes with one corrugation have been used for $\unicode[STIX]{x1D6FC}=0.5$ and $1$, boxes with five corrugation wavelengths have been used for $\unicode[STIX]{x1D6FC}=5$, and boxes with two, three and five wavelengths have been used for $\unicode[STIX]{x1D6FC}=3$.

Figure 22

Table 2.Variations of the flow rate as a function of time counted from the initiation of the instability determined from computations with $N$ Fourier modes and expressed as a fraction of the reference flow rate $Q_{ref}=4/3$ for channel with $\unicode[STIX]{x1D6FC}=3,S=0.125$ for $Re=600$ for instability initiated with vortices characterized by $\unicode[STIX]{x1D707}=2.25$.

Figure 23

Table 3.Variations of the mixing intensities defined by (4.1) and the flow rate $Q$ as functions of time counted from the initiation of the instability in a channel with $\unicode[STIX]{x1D6FC}=3$,$S=0.125$ for $Re=600$ and for the instability initiated with the vortices characterized by $\unicode[STIX]{x1D707}=2.25$ determined using $N=12$ Fourier modes.

Figure 24

Table 4.The same as table 3, but for $\unicode[STIX]{x1D6FC}=5,S=0.1$, $Re=1500$.

Figure 25

Figure 22.Variations of the kinetic energy (3.3) of the zeroth Fourier mode for flows through channel with $\unicode[STIX]{x1D6FC}=1,S=0.2$ at $Re=1000$. ,  and correspond to the two-dimensional oscillatory flow, the same flow modified with three-dimensional disturbance characterized by $\unicode[STIX]{x1D707}=2.25$ and the stationary flow modified with the same three-dimensional disturbance. $N=12$ Fourier modes have been used. Computational boxes containing one corrugation wavelength have been used in this study.

Figure 26

Table 5.The same as table 3, but for $\unicode[STIX]{x1D6FC}=1,S=0.2$, $Re=1000$.

Figure 27

Figure 23.Topology of the saturated flow field at $T=10^{4}$ for $\unicode[STIX]{x1D6FC}=1$, $S=0.2$, $Re=1000$. (a) The three-dimensional view of the $x$-component of the vorticity vector and (b) the $x$-direction view. (c) The enlargement of the bottom section of the above plot and (d) the side view of the enlargement; $N=12$ Fourier modes have been used in the computations.

Figure 28

Figure 24.Distributions of the $x$-component of the vorticity vector in the ($y,z$) plane overlaid with the vector lines of the ($y,z$) component of the velocity vector at (a) $x=0$, (b) $\unicode[STIX]{x1D706}/8$, (c) $\unicode[STIX]{x1D706}/4$, (d) $3\unicode[STIX]{x1D706}/8$, (e) $\unicode[STIX]{x1D706}/2$, (f) $5\unicode[STIX]{x1D706}/8$, (g) $3\unicode[STIX]{x1D706}/4$ and (h) $7\unicode[STIX]{x1D706}/8$. Arrows illustrate the ($y,z$) component of the velocity vector. Dashed lines separate zones with the positive and negative $x$-components of the vorticity vector. Flow and geometry conditions are the same as in figure 23.

Figure 29

Figure 25.Particle trajectories in the saturated flow field for $\unicode[STIX]{x1D6FC}=1,S=0.2$ at $Re=1000$. with the instability characterized by $\unicode[STIX]{x1D707}=2.25$. The $x$-direction has been scaled down 10 times. (a) The three-dimensional view, (b) view in the $z$-direction, (c) view in the $y$-direction, (d) view in the negative $x$-direction (only solid black and grey tracers are shown), (e) view in the negative $x$-direction (only dashed black and grey tracers are shown). Traces have been injected into the flow field at the narrowest section of the channel, near the bottom wall (solid black lines), at the mid-plane (solid grey lines) and near the top wall (dashed, black lines).

Figure 30

Table 6.Results of the grid convergence studies for the stationary two-dimensional flow with $Re=1500$ in a channel with $\unicode[STIX]{x1D6FC}=3$, $S=0.04$.

Figure 31

Figure 26.Variations of the complex amplification rate $\unicode[STIX]{x1D70E}$ as a function of the corrugation amplitude $S$ computed using the present method (thin solid line) and the IBC method (Floryan & Floryan 2010, thick grey lines) for $\unicode[STIX]{x1D6FC}=1$ and $Re=1000$.

Figure 32

Table 7.The amplification rate $\unicode[STIX]{x1D70E}_{i}$ for the vortex instability determined using different time steps during the simulation process. The comparison value has been determined by solving the relevant eigenvalue problem using the IBC method (Floryan 2003).

Figure 33

Figure 27.Variations of the critical conditions $(Re_{cr},\unicode[STIX]{x1D707}_{cr})$ for the vortex instability in a channel with the corrugation wavenumber $\unicode[STIX]{x1D6FC}=3$ as a function of the corrugation amplitude $S$ obtained using the present method as well as the IBC method. The IBC method provides continuous variations of the critical condition for $S\in (0,0.05)$ (dashed lines). The present method can be applied for any $S$ but provides results only at discrete values of $S$; the computed points are identified using symbols while the solid lines result from interpolation. Dotted lines identify extrapolated values. The box displays enlargement of the region where both methods are equally applicable.