InteriorSquirmer¶
Systems / ODEs / Climate & geophysics
The unsteady interior Stokes flow of an oscillating cylindrical squirmer, advecting tracers chaotically through a five-mode surface actuation.
Definition¶
\[
\begin{aligned}
\dot{r} &= 5 r^{4} \left(r^{2} - 1\right) \left(0.5 \left(0.5 - 0.5 \tanh{\left(20 \tau \sin{\left(\frac{2 \pi t}{\tau} \right)} \right)}\right) \cos{\left(5 \theta \right)} + 0.5 \left(0.5 \tanh{\left(20 \tau \sin{\left(\frac{2 \pi t}{\tau} \right)} \right)} + 0.5\right) \sin{\left(5 \theta \right)}\right) + 4 r^{3} \left(r^{2} - 1\right) \left(0.5 \left(0.5 - 0.5 \tanh{\left(20 \tau \sin{\left(\frac{2 \pi t}{\tau} \right)} \right)}\right) \cos{\left(4 \theta \right)} + 0.5 \left(0.5 \tanh{\left(20 \tau \sin{\left(\frac{2 \pi t}{\tau} \right)} \right)} + 0.5\right) \sin{\left(4 \theta \right)}\right) + 3 r^{2} \left(r^{2} - 1\right) \left(0.5 \left(0.5 - 0.5 \tanh{\left(20 \tau \sin{\left(\frac{2 \pi t}{\tau} \right)} \right)}\right) \cos{\left(3 \theta \right)} + 0.5 \left(0.5 \tanh{\left(20 \tau \sin{\left(\frac{2 \pi t}{\tau} \right)} \right)} + 0.5\right) \sin{\left(3 \theta \right)}\right) + 2 r \left(r^{2} - 1\right) \left(0.5 \left(0.5 - 0.5 \tanh{\left(20 \tau \sin{\left(\frac{2 \pi t}{\tau} \right)} \right)}\right) \cos{\left(2 \theta \right)} + 0.5 \left(0.5 \tanh{\left(20 \tau \sin{\left(\frac{2 \pi t}{\tau} \right)} \right)} + 0.5\right) \sin{\left(2 \theta \right)}\right) + \left(r^{2} - 1\right) \left(0.5 \left(0.5 - 0.5 \tanh{\left(20 \tau \sin{\left(\frac{2 \pi t}{\tau} \right)} \right)}\right) \cos{\left(\theta \right)} + 0.5 \left(0.5 \tanh{\left(20 \tau \sin{\left(\frac{2 \pi t}{\tau} \right)} \right)} + 0.5\right) \sin{\left(\theta \right)}\right) \\
\dot{theta} &= \frac{r^{5} \left(2 r + \frac{5 \left(r^{2} - 1\right)}{r}\right) \left(- 0.5 \left(0.5 - 0.5 \tanh{\left(20 \tau \sin{\left(\frac{2 \pi t}{\tau} \right)} \right)}\right) \sin{\left(5 \theta \right)} + 0.5 \left(0.5 \tanh{\left(20 \tau \sin{\left(\frac{2 \pi t}{\tau} \right)} \right)} + 0.5\right) \cos{\left(5 \theta \right)}\right) + r^{4} \left(2 r + \frac{4 \left(r^{2} - 1\right)}{r}\right) \left(- 0.5 \left(0.5 - 0.5 \tanh{\left(20 \tau \sin{\left(\frac{2 \pi t}{\tau} \right)} \right)}\right) \sin{\left(4 \theta \right)} + 0.5 \left(0.5 \tanh{\left(20 \tau \sin{\left(\frac{2 \pi t}{\tau} \right)} \right)} + 0.5\right) \cos{\left(4 \theta \right)}\right) + r^{3} \left(2 r + \frac{3 \left(r^{2} - 1\right)}{r}\right) \left(- 0.5 \left(0.5 - 0.5 \tanh{\left(20 \tau \sin{\left(\frac{2 \pi t}{\tau} \right)} \right)}\right) \sin{\left(3 \theta \right)} + 0.5 \left(0.5 \tanh{\left(20 \tau \sin{\left(\frac{2 \pi t}{\tau} \right)} \right)} + 0.5\right) \cos{\left(3 \theta \right)}\right) + r^{2} \left(2 r + \frac{2 \left(r^{2} - 1\right)}{r}\right) \left(- 0.5 \left(0.5 - 0.5 \tanh{\left(20 \tau \sin{\left(\frac{2 \pi t}{\tau} \right)} \right)}\right) \sin{\left(2 \theta \right)} + 0.5 \left(0.5 \tanh{\left(20 \tau \sin{\left(\frac{2 \pi t}{\tau} \right)} \right)} + 0.5\right) \cos{\left(2 \theta \right)}\right) + r \left(2 r + \frac{r^{2} - 1}{r}\right) \left(- 0.5 \left(0.5 - 0.5 \tanh{\left(20 \tau \sin{\left(\frac{2 \pi t}{\tau} \right)} \right)}\right) \sin{\left(\theta \right)} + 0.5 \left(0.5 \tanh{\left(20 \tau \sin{\left(\frac{2 \pi t}{\tau} \right)} \right)} + 0.5\right) \cos{\left(\theta \right)}\right)}{r} \\
\dot{t} &= 1
\end{aligned}
\]
Parameters¶
| Symbol | Default | Role |
|---|---|---|
tau |
3 |
surface-actuation period |
State variables: r, theta, t
Properties¶
Lyapunov spectrum
$+0.3539,\; -0.3556,\; 0$
computed at build
computed at build
Kaplan–Yorke dimension
$D_{KY} = 2.995$
Divergence ∇·f
n/a — too large to display — pathological rational divergence
Equilibria
none found (no equilibria)
Define it in TSDynamics¶
import tsdynamics as ts
sys = ts.systems.InteriorSquirmer()
traj = sys.integrate(final_time=100.0, dt=0.01)
exps = sys.lyapunov_spectrum()
ts.kaplan_yorke_dimension(exps)
Reference¶
Blake (1971), Bull. Aust. Math. Soc. 5, 255-264
