Only depends on position. Taking the curl,
The field reverses across . Its divergence is zero, as required for a magnetic field; the vanishing field on the midplane is important for the crossing and separatrix trajectories below.
With zero scalar potential, the nonrelativistic charged-particle Lagrangian in SI units is kinetic energy plus . Thus
The velocity-dependent magnetic term changes canonical momentum but does not contribute to the mechanical energy.
Define . Differentiating the Lagrangian with respect to each generalized velocity gives
The coordinates and are cyclic, so and are conserved. The momentum is generally not conserved: its equation is . In particular, conserved canonical is not the same as conserved mechanical , which changes as the particle moves across the magnetic-field gradient.
The Legendre transform cancels the term linear in velocity and gives
It equals the mechanical kinetic energy. The Hamiltonian has no explicit time dependence, so is conserved. This is also a direct consequence of the magnetic force doing no work: .
Since initially and remains constant, the motion stays in a plane of constant . Setting and gives
The allowed interval obeys . The sign of is set by the initial direction and changes at a turning point. The specified fixes the starting position on the energy orbit, but the data do not specify which sign of the initial transverse velocity is chosen.
Dividing the two velocities gives
Here : the orbit always advances toward increasing , except for instantaneous zeros at each midplane crossing . The transverse motion oscillates between and . At these outer turning points and the trajectory is tangent to the direction; at the midplane while , so the tangent is along . The sign of the initial only chooses the phase or reflected trace.
Figure 1.
Crossing and separatrix orbits in a reversing magnetic field
. The left panel shows the orbit with zero conserved axial canonical momentum, advancing monotonically in z. The right panel shows a positive-x separatrix with the negative extreme canonical momentum; its arrows and marked axial-velocity zeros distinguish it from an ordinary periodic orbit. Both panels use dimensionless coordinates. Details.
With , the allowed range is , where . But an orbit starting with never crosses the midplane in finite time, because
One positive-side separatrix, with and , is
The negative-side orbit is its reflection in . For the positive branch, rises from zero asymptotically, reaches at , then returns asymptotically to zero. Thus the infimum is zero but it is not attained in finite time on this nontrivial branch. Since , the two axial-velocity zeros occur at . Motion is toward decreasing near either asymptotic midplane tail and toward increasing near the outer excursion. These directions are marked in part i.
The exactly midplane initial state , is a separate straight trajectory with ; it must not be described as a finite-time crossing of the separatrix.
Differentiation gives
The angles and are cyclic, so their canonical momenta are conserved. The Lagrangian is autonomous, so the total energy is also conserved. The momentum is not generally constant because gravity and the angular kinetic terms depend on .
At the initially vertical configuration, the two conserved momenta coincide:
The apparent angular term at is interpreted by its regular limit with these equal momenta. Substitution into energy conservation, followed by , gives
Writing yields
The zero of the potential at the vertical configuration includes the initially specified transverse kinetic energy separately as .
Use the conserved in the canonical-momentum equation. For a nonzero tilt,
Cancelling with the half-angle identities gives
Its regular limit at the north pole is , although the azimuth itself is not a uniquely defined coordinate at that pole.
Put . Then . For it increases from zero at the north pole to infinity as and has no interior minimum. The vertical orientation is stable. Near zero,
For , away from the marginal case , this gives
The locally signed tilt oscillates at angular frequency , while the azimuth precesses approximately at . The nonnegative polar coordinate is , so its successive pole-to-pole excursions have period and angular repetition frequency . Stating this convention avoids confusing a signed small displacement with the polar-angle magnitude. The full axis direction combines that excursion with precession.
Figure 1.
The vertical spinning top changes from a stable minimum to an unstable maximum
. Dimensionless effective potentials are shown for alpha equal to 0.5 and 2. The second panel marks the off-axis minimum and the zero-energy turning angle approached by a near-separatrix excursion. Details.
For , is an unstable stationary point and the interior minimum satisfies . Hence
The potential then diverges at . For , the turning point is specified exactly by the smaller quadratic root
For small positive , this approaches , a finite excursion even when the initial impulse is arbitrarily small. An excursion from the north pole to the outer turning angle and back has period
Near the unstable pole, with . The near-pole contribution gives , so the period diverges logarithmically as . The exactly unperturbed top can remain at the unstable vertical orientation; the limiting excursions spend ever longer close to it. The direction also precesses according to part c.
For each canonical coordinate and momentum, Hamilton's equations are
They use canonical rather than arbitrary mechanical momenta, a distinction important in a magnetic field. The bracket convention printed in the source is consistent with for a function with no explicit time dependence.
Apply the chain rule to the phase-space function:
Thus . If an explicitly time-dependent function is allowed, the correct equation is , so a vanishing bracket alone would not suffice. The source specifies , for which that extra term is absent.
The radial and azimuthal Hamilton equations give
Also and . Differentiating the angular-momentum square,
Therefore both and are constants. Rotational symmetry conserves the full angular-momentum vector; these are its axial component and squared magnitude in spherical canonical variables.
In the equatorial plane,
Differentiating the given combination produces a cosine term
and a sine term . Thus . The expression is a Cartesian component of the Laplace-Runge-Lenz vector with a conventional overall normalization, reflecting the additional symmetry of the inverse-square-force problem.
With the apsidal origin chosen as specified, . For , rearrangement gives
Let . Since , the equation is . Its solution, continued through points where the intermediate division fails, is
As printed, has units of inverse length and is not the usual dimensionless eccentricity. Writing gives the standard form with . The orbit is an ellipse for , parabolic for unit magnitude and hyperbolic for magnitude greater than one on its allowed angular interval. The purely radial case must be handled separately and is excluded by these divisions.

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