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Vortex-induced vibrations: a soft coral feeding strategy?

Published online by Cambridge University Press:  14 April 2021

Mouad Boudina*
Affiliation:
Department of Mechanical Engineering, Polytechnique Montréal, Montréal, H3T 1J4 Québec, CanadaLaboratory for Multiscale Mechanics (LM2), Polytechnique Montréal, Montréal, H3T 1J4 Québec, Canada
Frédérick P. Gosselin
Affiliation:
Department of Mechanical Engineering, Polytechnique Montréal, Montréal, H3T 1J4 Québec, CanadaLaboratory for Multiscale Mechanics (LM2), Polytechnique Montréal, Montréal, H3T 1J4 Québec, Canada
Stéphane Étienne
Affiliation:
Department of Mechanical Engineering, Polytechnique Montréal, Montréal, H3T 1J4 Québec, Canada
*
†Email address for correspondence: mouad.boudina@polymtl.ca

Abstract

Soft corals, such as the bipinnate sea plume Antillogorgia bipinnata, are colony building animals that feed by catching food particles brought by currents. Because of their flexible skeleton, they bend and sway back and forth with the wave swell. In addition to this low-frequency sway of the whole colony, branches of A. bipinnata vibrate at high frequency with small amplitude and transverse to the flow as the wave flow speed peaks. In this paper, we investigate the origin of these yet unexplained vibrations and consider their effect on soft corals. Estimation of dynamical variables along with finite element implementation of the wake-oscillator model favour vortex-induced vibrations (VIVs) as the most probable origin of the observed rapid dynamics. To assess the impact of the dynamics on filter feeding, we simulated particles advected by the flow around a circular cylinder and calculated the capture rate with an in-house monolithic fluid–structure interaction (FSI) finite element solver and Python code. We observe that vibrating cylinders can capture up to 40 % more particles than fixed cylinders at frequency lock-in. Therefore, VIVs plausibly offer soft corals a better food capture.

Information

Type
JFM Papers
Copyright
© The Author(s), 2021. Published by Cambridge University Press
Figure 0

Figure 1.(a) Schematic of a bipinnate sea plume A. bipinnata swaying back and forth under surface wave action, with branches exhibiting small and rapid transverse vibrations. The coral colony stands perpendicular to the flow and encounters incoming food particles. (b) Cross-section of a branch vibrating, owing to the vortex shedding in the wake, and facing two incoming particles. The upper particle crosses over the branch and escapes capture, whereas the lower particle approaches the branch surface and gets intercepted. (c) Schematic summary of the numerical results of the particle capture efficiency, as defined in (1.1), versus flow speed. The soft coral branch maximises the efficiency of particle capture during the lock-in phase, where the vortex shedding frequency synchronises with the natural frequency of the branch. Art by IMPAKT Scientifik.

Figure 1

Figure 2.Numerical deformation profiles of elastic rods of lengths $L = 1$, 5 and 8 cm subjected to VIVs in a unidirectional flow. The vertical line in the left of each case indicates the initial configuration of the rod. On the middle and the right are the lateral and frontal profiles, respectively. The lengths are proportional. In the online record of the vibrating soft coral, we also see small branches staying relatively straight and having a first mode vibration, and longer branches reconfiguring more with the flow and having a second mode vibration with a single zero-displacement node.

Figure 2

Figure 3.Dried bipinnate sea plume Antillogorgia bipinnata (Nova South Eastern University (2016), © Charles G. Messing). The centre-to-centre separation space between branches goes from 4.5 to 8.5 diameters. The cortex of some polyps can be discerned in the extremities of the branches (top left, bottom left and bottom right of the image).

Figure 3

Figure 4.(a) Schematics of particles advected by a flow around a cylinder free to oscillate in the transverse and stream-wise directions. The upstream fluid velocity is parallel to $\boldsymbol {e}_{x}$. Particles have a density $\rho _{p}$ and diameter $d_{p}$. The mass per unit length of the cylinder is $m$, and the spring stiffness per unit length $k$ is the same in both directions. (b) Drawing contrasting the size of particles simulated with the size of the cylinder, where $R = d_{p}/D$ is the diameter ratio.

Figure 4

Figure 5.Close-ups of the fluid mesh highlighting the densification in the wake (a) and around the boundary layer (b).

Figure 5

Figure 6.Schematics of particle interception by a fixed cylinder. Particles are launched from a distance $x_{0}$ upstream from the cylinder. Because the blue particle starts near the symmetry line, it is captured, whereas the red particle starts from a higher $y$-position and succeeds in crossing over the cylinder and escaping capture. The grey particle is the farthest particle from the symmetry line that the cylinder intercepts. Its trajectory starts from the ordinate $y^+$, and defines the upper border of the capture domain. The size of the capture window is $w = y^+ - y^{-}$.

Figure 6

Figure 7.Distortion of the capture domain owing to vibration. The initial ordinates of the grey border particles are now varying in time $y^{\pm } = y^{\pm }(t)$. The instantaneous capture window, through which the particles launched at time $t$ would be captured, is $w(t) = y^+(t) - y^{-}(t)$. At instants $t$ between $t_{1}$ and $t_{2} > t_{1}$, the blue particles are launched between $y^{-}(t)$ and $y^+(t)$, so they are captured. The red particles are launched outside of these limits, so they escape capture. A portion of particle trajectories is shown by the solid line. The cylinder draws a lemniscate trajectory, and $Y_{max}$ and $X_{max}$ are the transverse and stream-wise amplitudes of vibration. The motion of the cylinder is symmetric with respect to the horizontal line passing through the node of the lemniscate, hence the capture is periodic and goes in harmony with the stream-wise oscillations, which complete a cycle in half a period.

Figure 7

Figure 8.Mean capture rate $\langle \eta \rangle$ versus the reduced velocity for (a) the particle of diameter ratio $R = 0.031$, and for (b) all particles $0.015 \le R \le 0.1$ in flows of Reynolds numbers $50 \le {\textit{Re}} \le 200$. In (b), the $y$-axis is logarithmic, and each group of four curves with a single grey level corresponds to the particles $R = 0.015$ (white), 0.031 (light grey), 0.05 (grey) and 0.1 (black).

Figure 8

Figure 9.Mean capture rate of the fixed cylinder ($\circ$, black) and the vibrating cylinder ($\triangle$, green, $U_{r} = 5$ and $\triangledown$, red, $U_{r} = 13$) versus the product $R^{2}{\textit{Re}}^{1/2}$. For $R^{2}{\textit{Re}}^{1/2} \lesssim 0.06$, the capture rate varies as $\langle \eta \rangle \sim \langle \eta \rangle _{fixed} \sim R^{2}{\textit{Re}}^{1/2}$. Beyond this value, the scaling deviates to $R^{2}{\textit{Re}}$, as indicated by the dash–dotted line (–$\cdot$–).

Figure 9

Figure 10.Variation of the gain in capture rate versus the reduced velocity for all simulation cases $0.015 \le R \le 0.1$ and $50 \le {\textit{Re}} \le 200$.

Figure 10

Table 1.The peak value of the gain in capture $\delta$ for each Reynolds number ${\textit{Re}}$.

Figure 11

Figure 11.Numerical response of (a) the transverse and (b) the stream-wise amplitudes of the cylinder.

Figure 12

Figure 12.Variation of the gain in capture rate versus the transverse and stream-wise amplitudes of the cylinder for all simulation cases $0.015 \le R \le 0.1$ and $50 \le {\textit{Re}} \le 200$. The $x$-axis in (b) is logarithmic to visualise better the staggered data points.

Figure 13

Figure 13.Shape of the lemniscate limit-cycle trajectory of the cylinder in a flow at $Re = 100$ versus the reduced velocity. The $x$-span of each lemniscate is magnified by approximately 13 times to elucidate the loops.

Figure 14

Figure 14.(a) Slenderness ratio of the lemniscate limit-cycle trajectory of the cylinder versus the reduced velocity for the Reynolds numbers $50 \le {\textit{Re}} \le 200$. For low reduced velocities, $\gamma$ starts from a relatively small value and decreases until it reaches the minimum at lock-in ($U_{r} \approx 5$). From $U_{r} = 1$ to 8, the slenderness ratio for all Reynolds numbers follows the same trend. Beyond $U_{r} = 8$, it keeps increasing for ${\textit{Re}} = 50$, while it plateaus for $100 \le {\textit{Re}} \le 200$. (b) Gain in capture rate versus the slenderness ratio of the lemniscate for all simulation cases $0.015 \le R \le 0.1$ and $50 \le {\textit{Re}} \le 200$. For $\gamma < 40$, data points converge around two branches. The lower branch, which is close to the zero value, corresponds to low reduced velocities, whereas the upper branch represents the region around lock-in. The dashed line in both graphics is the critical value $\gamma ^{*} = 40$ cutting the domain in two regions: extended lemniscates for $\gamma < 40$ and thin lemniscates for $\gamma > 40$.

Figure 15

Figure 15.(a) Vorticity contour plot of a flow around an idealised soft coral cross-section at the angle of attack 20$^{\circ }$ and Reynolds number ${\textit{Re}} = 200$. The cross-section is a circle and polyps are the two diametrically opposed arcs of a circle. Their size is 10 % of the circle diameter. (b) Mean values of the fluctuating drag and lift coefficients, $C_{D}$ ($\square$, red) and $C_{L}$ ($\square$, blue). The bars refer to the maximum and minimum values of the variables. The mean value of $\mathrm {d}C_{L}/\mathrm {d}\alpha + C_{D}$ ($\circ$, green) is calculated from cubic spline interpolation of the data points.

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