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Transient growth analysis of hypersonic flow over an elliptic cone

Published online by Cambridge University Press:  03 February 2022

Helio Quintanilha Jr.*
Affiliation:
School of Engineering, University of Liverpool, The Quadrangle, Liverpool L69 3GH, UK
Pedro Paredes
Affiliation:
National Institute of Aerospace, Hampton, VA 23666, USA
Ardeshir Hanifi
Affiliation:
Department of Engineering Mechanics, KTH Royal Institute of Technology, FLOW and Swedish e-Science Research Centre (SeRC), 100 44 Stockholm, Sweden
Vassilis Theofilis
Affiliation:
School of Engineering, University of Liverpool, The Quadrangle, Liverpool L69 3GH, UK Escola Politécnica, Universidade São Paulo, Av. Prof. Mello Moraes 2231, CEP 5508-900, São Paulo-SP, Brasil
*
†Email address for correspondence: hquintanilhajr@gmail.com

Abstract

Non-modal linear stability analysis results are presented for hypersonic flow over an elliptic cone with an aspect ratio of two at zero angle of attack, completing earlier modal instability analysis of flow around the same geometry. The theoretical framework to perform transient growth analysis of compressible flows on a generalized two-dimensional frame of reference is developed for the first time and is then applied to solve the initial-value problem governing non-modal linear instability on planes perpendicular to the cone axis, taken at successive streamwise locations along the elliptic cone. Parameter ranges examined here are chosen so as to model flight of the Hypersonic International Flight Research Experimentation 5 (HIFiRE-5) test geometry at altitudes of 21 km and 33 km, corresponding to Mach numbers 7.45 and 8.05 and unit Reynolds numbers $Re' = 1.07\times 10^7$ and $1.89\times 10^6$, respectively. Results obtained indicate that the significance of the non-modal growth for laminar–turbulent transition increases with increasing flight altitude (decreasing Reynolds number). At a given set of flow parameters, transient growth is stronger in the vicinity of the tip of the cone and in azimuthal locations away from both of the minor (centreline) and major (attachment line) axes of the cone. Linear optimal disturbances calculated at conditions of maximal transient growth are found to peak in the crossflow region of the elliptic cone. These structures are elongated along the streamwise spatial direction, while being periodic along the spanwise direction with periodicity lengths of the same order of magnitude as the well-known structures identified as crossflow vortices in both experiments and simulations.

Information

Type
JFM Papers
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited.
Copyright
© The Author(s), 2022. Published by Cambridge University Press
Figure 0

Figure 1. Example of the two domains used to perform the global stability analysis. The first domain is covering the centreline and the crossflow region (${\rm \pi} /2 \leq \zeta \leq {\rm \pi}/4$), whereas the second domain accounts for the region close to the attachment line ($\zeta = 0$).

Figure 1

Table 1. Flow conditions for both altitudes analysed in this paper.

Figure 2

Figure 2. Mach number contours of the base flow at 33 km altitude and $x^* = 0.36$ m. (a) Two-dimensional base flow used in the global stability analysis; (b) one-dimensional base flow used in the local stability analysis.

Figure 3

Figure 3. Comparison of the energy growth $G(t)$ for the three different grids analysed. The energy growth curves were obtained at (a) 21 km and (b) 33 km altitude, with $\alpha =0.11$ and at $x^* = 0.36$ m. The dashed line represents the slope of the most unstable eigenvalue calculated from the EVP analysis.

Figure 4

Figure 4. Streamwise velocity magnitude $\|\hat {u}\|$ of the leading symmetric (a) and antisymmetric (b) centreline modes at $x^*=0.52$ m. The black lines are isocontours of the base flow ($\bar {u} = 0:(0.1):0.9$).

Figure 5

Figure 5. Streamwise velocity magnitude $\|\hat {u}\|$ of the leading symmetric (a) and antisymmetric (b) attachment line modes at $x^*=0.52$ m. The black lines are isocontours of the base flow ($\bar {u} = 0$ and 0.9).

Figure 6

Figure 6. Contours of energy gain $G(t)$ varying streamwise $\alpha$ and spanwise $\beta$ wavenumbers: (a,b) 21 km altitude; (c,d) 33 km altitude.

Figure 7

Figure 7. Comparison of transient growth at 21 km and 33 km altitudes with $\alpha = 0$ at streamwise locations (a) $x^* = 0.36$ m, (b) $x^* = 0.42$ m, (c) $x^* = 0.52$ m, and (d) $x^* = 0.62$ m.

Figure 8

Figure 8. Best fit of the gain function at $t = t_{opt}$ as a function of $Re_x$: (a) 21 km altitude quadratic fit; (b) 33 km altitude quartic fit.

Figure 9

Figure 9. Real part of perturbation density $\hat {\rho }_r$ with $\alpha =0$. The first column (a–e) corresponds to the optimal initial condition $t=0$; the middle column ( f–j) corresponds to the associated optimal perturbation $t=t_{opt}$; and the right column (k–o) corresponds to the long time behaviour $t \rightarrow \infty$. Each row corresponds to a different streamwise location along the elliptic cone surface, namely $x^* = 0.36$ m (a, f,k), $x^* = 0.42$ m (b,g,l), $x^* = 0.52$ m (c,h,m), $x^* = 0.62$ m (d,i,n) and $x^* = 0.72$ m (e,j,o). The black isolines correspond to contours of the steady base flow ($\bar {u} = 0$ and 0.95).

Figure 10

Figure 10. Real part of streamwise perturbation $\hat {u}_r$ with $\alpha =0$. The first column (a–e) corresponds to the optimal initial condition $t=0$; the middle column ( f–j) corresponds to the associated optimal perturbation $t=t_{opt}$; and the right column (k–o) corresponds to the long time behaviour $t \rightarrow \infty$. Each row corresponds to a different streamwise location along the elliptic cone surface, namely $x^* = 0.36$ m (a, f,k), $x^* = 0.42$ m (b,g,l), $x^* = 0.52$ m (c,h,m), $x^* = 0.62$ m (d,i,n) and $x^* = 0.72$ m (e,j,o). The black isolines correspond to contours of the steady base flow ($\bar {u} = 0$ and 0.95).

Figure 11

Table 2. Relationship between $G(t_{opt})$ and the different axial locations and respective $Re_x$ values along the elliptic cone model for both 21 km and 33 km altitudes.

Figure 12

Figure 11. Top view of the elliptic cone model. (a) Oil flow visualization of experimental crossflow modes reported by Borg et al. (2012) at $Ma = 6$ and $Re' = 8.1 \times 10^6$ m$^{-1}$. (b) Three-dimensional reconstruction of the linear optimal streamwise velocity component calculated at 33 km altitude, $Ma = 8.05$, $Re' = 1.89 \times 10^6$ m$^{-1}$ and $\alpha = 0$.

Figure 13

Figure 12. Comparison of energy gain between 21 km and 33 km altitudes with $\alpha =0.2$ for different streamwise positions: (a) $x^* = 0.36$ m, (b) $x^* = 0.42$ m, (c) $x^* = 0.52$ m, and (d) $x^* = 0.62$ m.

Figure 14

Figure 13. Real part of perturbation density $\hat {\rho }_r$ with $\alpha =0.2$ ($L_x = 16.1$ mm). The first column (a–d) corresponds to the optimal initial condition $t=0$; the middle column (e–h) corresponds to the associated optimal perturbation $t=t_{opt}$; and the right column (i–l) corresponds to the long time behaviour $t \rightarrow \infty$. Each row corresponds to a different streamwise location along the elliptic cone surface, namely $x^* = 0.36$ m (a,e,i), $x^* = 0.42$ m (b, f, j), $x^* = 0.52$ m (c,g,k) and $x^* = 0.62$ m (d,h,l). The black isolines correspond to contours of the steady base flow ($\bar {u} = 0$ and 0.95).

Figure 15

Figure 14. Real part of streamwise perturbation $\hat {u}_r$ with $\alpha =0.2$ ($L_x=16.1$ mm). The first column (a–d) corresponds to the optimal initial condition $t=0$; the middle column (e–h) corresponds to the associated optimal perturbation $t=t_{opt}$; and the right column (i–l) corresponds to the long time behaviour $t \rightarrow \infty$. Each row corresponds to a different streamwise location along the elliptic cone surface, namely $x^* = 0.36$ m (a,e,i), $x^* = 0.42$ m (b,f,j), $x^* = 0.52$ m (c,g,k) and $x^* = 0.62$ m (d,h,l). The black isolines correspond to contours of the steady base flow ($\bar {u} = 0$ and 0.95).

Figure 16

Figure 15. (a) Gain $G(t)$ calculated via SVD (solid lines) compared with the slope of the most unstable eigenvalue calculated via the EVP analysis (dashed lines) at $x^* = 0.52$ m and 33 km altitude. (b) The associated $\omega _i$ vs $\alpha$ curve showing the modally unstable region.