Bertrand's theorem
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In classical mechanics, Bertrand's theorem states that only two types of potentials produce stable, closed orbits: an inverse-square force such as the gravitational or electrostatic potential
- [V(\mathbf) = \frac]
- [V(\mathbf) = \frac kr^]
General Preliminaries
All attractive central forces can produce closed, circular orbits; all that's required is to match the force with the centripetal force requirement and calculate the required angular velocity. Non-central forces (i.e., those that depend on the angular variables as well as the radius) do not produce circular orbits in general, so we ignore them here.
The equation of motion for the radius [r] of a particle of mass [m] moving in a central potential [V(r)] is given by Lagrange's equations
- [m\fracr}} - mr \omega^ = m\fracr}} - \frac}} = -\frac]
The angular-momentum definition allows a change of independent variable from [t] to [\theta]
- [\frac = \frac} \frac]
- [\frac} \frac \left( \frac} \frac \right)- \frac}} = -\frac]
- [\fracu}} + u = -\frac} \frac V(1/u)]
Bertrand's theorem
As noted above, all central forces can produce closed, circular orbits given an appropriate initial velocity. However, these orbits need not be stable (i.e., remain in orbit indefinitely if some radial velocity is introduced) nor closed (repeatedly returning to exactly the same path). Here we show that stable, exactly closed orbits can be produced only with an inverse-square force or radial harmonic oscillator potential (a necessary condition). In the following sections, we show that those force laws do produce stable, exactly closed orbits (a sufficient condition).
For brevity, we introduce the function [J(u)] into the equation for [u]
- [\fracu}} + u = J(u) \equiv -\frac} \frac V(1/u) = -\fracu^} f(1/u)]
- [
where [u_ \equiv 1/r_].
The next step is to consider the equation for [u] under small perturbations [\eta \equiv u - u_] from perfectly circular orbits. On the right-hand side, the [J] function can be expanded in a standard Taylor series
- [J(u) \approx u_ + \eta J^(u_) + \frac \eta^ J^(u_) + \frac \eta^ J^(u_) + \ldots]
- [\frac\eta}} + \eta = \eta J^(u_) + \frac \eta^ J^(u_) + \frac \eta^ J^(u_) \ldots]
- [\frac\eta}} + \beta^ \eta = \frac \eta^ J^(u_) + \frac \eta^ J^(u_) \ldots]
- [\eta(\theta) = h_ \cos \beta\theta]
- [J^(u_) \equiv -2 + \frac})} \frac = 1 - \beta^ ]
- [\frac = \left( \beta^ - 3 \right) \frac]
- [f(r) = - \frac}}]
- [J(u) = \frac} u^}]
For more general deviations from circularity (i.e., when we cannot neglect the higher order terms in the Taylor expansion of [J]), [\eta] may be expanded in a Fourier series, e.g.,
- [\eta(\theta) = h_ + h_ \cos \beta \theta + h_ \cos 2\beta \theta + h_ \cos 3\beta \theta + \ldots]
- [h_ = h_^ \frac(u_)}}]
- [h_ = -h_^ \frac(u_)}}]
- [h_ = -\frac} \left[ h_h_ frac(u_)} +h_^ frac(u_)} right]]
- [ \left( 2 h_ h_ + h_ h_ \right) \frac(u_)} + h_^ \frac(u_)} = 0]
- [\beta^ \left( 1 - \beta^ \right) \left( 4 - \beta^ \right) = 0]
Inverse-square force (Kepler problem)
For an inverse-square force law such as the gravitational or electrostatic potential, the potential can be written
- [V(\mathbf) = \frac = -ku]
The orbit [u(\theta)] can be derived from the general equation
- [\fracu}} + u = -\frac} \frac V(1/u) = \frac}]
- [
where [e] (the eccentricity) and [\theta_] (the phase offset) are constants of integration.
This is the general formula for a conic section that has one focus at the origin; [e=0] corresponds to a circle, [e<1] corresponds to an ellipse, [e=1] corresponds to a parabola, and [e>1] corresponds to a hyperbola. The eccentricity [e] is related to the total energy [E] (cf. the Laplace-Runge-Lenz vector)
- [
Comparing these formulae shows that [E<0] corresponds to an ellipse, [E=0] corresponds to a parabola, and [E>0] corresponds to a hyperbola. In particular, [E=-\fracm}}] for perfectly circular orbits.
Radial harmonic oscillator
To solve for the orbit under a radial harmonic oscillator potential, it's easier to work in components [\mathbf = (x, y, z)]. The potential energy can be written
- [V(\mathbf) = \frac kr^ = \frac k \left( x^ + y^ + z^\right)]
- [\fracx}} + \omega_^ x = 0]
- [\fracy}} + \omega_^ y = 0]
- [\fracz}} + \omega_^ z = 0]
- [x = A_ \cos \left(\omega_ t + \phi_ \right)]
- [y = A_ \cos \left(\omega_ t + \phi_ \right)]
- [z = A_ \cos \left(\omega_ t + \phi_ \right)]
- [T \equiv \frac}]
Reference
- Goldstein H. (1980) Classical Mechanics, 2nd. ed., Addison-Wesley. ISBN 0201029189
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