precession of the equinoxes

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Let us suppose an extended body body of mass m\, is in a circular orbit around a distant body of mass M\,, and let us choose, at an instant in time, a body-fixed basis \mathbf{\hat{x}}_b,\mathbf{\hat{y}}_b,\mathbf{\hat{z}}_b\, in which the moment of inertia tensor \mathbf{I}\, is diagonal.

Furthermore, choose spherical coordinates such that the distant mass M\, be located in the direction

\hat\mathbf{r} = \sin\xi \cos\zeta\mathbf{\hat{x}}_b + \sin\xi \sin\zeta\mathbf{\hat{y}}_b + \cos\xi \mathbf{\hat{z}}_b\,,

at a distance r\,, where \xi\, is the angle subtended between \hat{\mathbf{z}}_b\, and \hat\mathbf{r}\,. The moment of inertia about an axis \hat\mathbf{r}\, is I_r = \hat\mathbf{r}^T \mathbf{I} \hat\mathbf{r}\,, so

I_{r} = (\sin\xi\cos\zeta)^2 I^{b}_{xx} + (\sin\xi \sin\zeta)^2 I^b_{yy} + (\cos\xi)^2 I^b_{zz}\,.

Let us further suppose that I_{xx} = I_{yy}\, so that

I_{r} = I^{b}_{xx} \sin^2\xi + \cos^2\xi I^b_{zz}\,,

and (dropping the superscript b\,), the gravitational potential energy is

V\,  = -\frac{GMm}{r} + \frac{GM}{2 r^3} \left(I_{xx} - I_{zz} \right) \left(1 - 3 \cos^2\xi\right)\,,
 = -\frac{GMm}{r} - \frac{GM}{r^3} \left(I_{xx} - I_{zz} \right) P_2(\cos\xi)\,.

Now, in space axes aligned with the ecliptic, \hat\mathbf{z}_b = \sin\theta \sin\psi\hat\mathbf{x} +\sin\theta\cos\psi\hat\mathbf{y} +  \cos\theta \hat\mathbf{z}\,, \hat\mathbf{r} = \cos\eta \hat\mathbf{x} - \sin\eta \hat\mathbf{y}\,, so that \cos\xi = -\sin\theta \sin(\eta-\psi)\,. Normally precession happens over a time scale much slower than the orbital motion. If we average over one period,

\frac{1}{2\pi}\int\!d\eta\, P_2(\cos\xi) = \frac{1}{2}\left( \tfrac{3}{2}\sin^2\theta -1\right)\,,

so that

\left\langle V \right\rangle = -\frac{GMm}{2r} - \frac{GM}{2r^3} \left(I_{xx} - I_{zz} \right) \left( \tfrac{3}{2}\sin^2\theta -1\right)\,.

The angular velocity in a body-fixed basis in terms of Euler angles is

\boldsymbol{\omega} = 
\begin{pmatrix}
\omega_{x_b}\\
\omega_{y_b}\\
\omega_{z_b}
\end{pmatrix}=
\begin{pmatrix}
\sin\psi \sin\theta \dot{\phi} + \cos\psi \dot\theta\\
\cos\psi \sin\theta \dot{\phi} - \sin\psi \dot\theta\\
\cos\theta \dot{\phi} + \dot\psi
\end{pmatrix}\,,

so the kinetic energy T = \tfrac{1}{2} \boldsymbol{\omega}^T I \boldsymbol{\omega}\, is

T = \frac{1}{2}I_{xx} ( \sin^2\theta \dot{\phi}^2 + \dot{\theta}^2 ) + \frac{1}{2}I_{zz} (\cos\theta \dot\phi + \dot\psi)^2\,,

and the effective Lagrangian governing precession is

L = \frac{1}{2}I_{xx} ( \sin^2\theta \dot{\phi}^2 + \dot{\theta}^2 ) + \frac{1}{2}I_{zz} (\cos\theta \dot\phi + \dot\psi)^2 - \frac{GM}{ 2r^3} \left(I_{xx}- I_{zz} \right) \left(1 -\tfrac{3}{2}  \sin^2\theta \right)\,.

Since \frac{\partial L}{\partial \psi} = 0\,, we see that \Omega = \cos\theta \dot\phi + \dot\psi\, is an integral of motion, and

L = \frac{1}{2}I_{xx} ( \sin^2\theta \dot{\phi}^2 + \dot{\theta}^2 ) +\frac{1}{2} I_{zz} \Omega^2 - \frac{GM}{ 2r^3} \left(I_{xx}- I_{zz} \right) \left(1 -\tfrac{3}{2}  \sin^2\theta \right)\,.

Then

\frac{d}{dt} \frac{\partial L}{\partial \dot{\theta}} - \frac{\partial L}{\partial \theta} = I_{xx} \ddot{\theta} - \frac{\partial L}{\partial \theta} = 0\,.

For steady precession, \dot{\phi} = 0\,, so

\frac{\partial L}{\partial \theta} = I_{xx} \sin\theta\cos\theta \dot{\phi}^2 - I_{zz} \Omega \sin\theta \dot{\phi} + \frac{GM}{2r^3} (I_{xx} - I_{zz})(3\sin\theta\cos\theta) = 0\,,

or

I_{xx} \cos\theta \dot{\phi}^2 - I_{zz} \Omega  \dot{\phi} + \frac{GM}{2r^3} (I_{xx} - I_{zz})(3\cos\theta) = 0\,.

Assuming \dot\phi \ll \Omega\,,

\dot{\phi} \approx - \frac{GM}{2\Omega r^3}\frac{ (I_{zz} - I_{xx}) }{I_{zz}} (3\cos\theta) \,.
back to gravitational potential of an extended body
back to Gravitational potential theory

References

Further reading:[1] [2] [3]

  1. Landau, L.D.; Lifshitz, E.M. (1997). Mechanics (3rd ed). Butterworth-Heinemann. ISBN 0-750-62896-0. 
  2. Herbert Goldstein, Charles P. Poole, John L. Safko (1980). Classical Mechanics (3rd ed). Addison Wesley. ISBN 978-0201657029. 
  3. Richard Fitzpatrick, Classical Dynamics: An intermediate level course, retrieved October 16, 2007
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