In cylindrical coordinates the orthogonal velocity components are , , . Their squared magnitudes add, and . Thus . Taking the curl gives , consistent with the prescribed field.
Velocity differentiation gives . The coordinates and are cyclic, so are conserved. The radial momentum generally changes. In particular the conserved axial canonical momentum differs from the axial mechanical momentum by .
The Legendre transform cancels the velocity-linear magnetic term. Expressing velocities in terms of momenta gives
The Hamiltonian is time independent and hence conserved. It equals kinetic energy because a static magnetic field does no work; its dependence on is through the mechanical momentum combination.
The initial condition makes at all times. Accessible radii obey . For and , monotonicity of gives exactly the two stated turning equations and confinement to the interval between their unique roots.
The squared condition alone omits a sign qualification. More generally both positive roots require , and are the sorted roots . For example , , , confines the orbit to , but the source's named equations reverse those labels. This is a convention issue, not a failure of confinement.
Expand about . Then and conservation of energy gives
Here can be signed, but the physical oscillation frequency and amplitude are nonnegative. The small-energy condition ensures that this local expansion samples only a narrow range about , provided the field varies smoothly there.
Use rotating basis vectors with , . The inertial velocity is . The two fixed rotating anchors are , so the spring lengths are . Combining kinetic and elastic energies gives
A constant elastic offset has no dynamical effect.
Differentiate the quadratic Lagrangian with respect to coordinates and velocities. The equations are
The velocity-cross terms are Coriolis accelerations; moving to the force side identifies the outward centrifugal acceleration. The remaining terms are elastic restoring forces. The sign pair is fixed by the rotating-basis convention in part a.
Substitution of the exponential ansatz gives the homogeneous amplitude system
A nonzero mode requires zero determinant. Thus with the stated two effective stiffnesses. The off-diagonal product is positive, which determines the sign on the right.
Put and . Its equation is . If both effective stiffnesses are positive, the sum and product of roots are positive and , so both roots are positive. They can coincide in a degenerate zero-rotation isotropic case; “two” need not mean distinct.
If , the product is negative, so one root is negative. Its imaginary frequency gives a growing exponential displacement: centrifugal softening has overwhelmed one elastic restoring direction, making the central configuration unstable. Coriolis coupling mixes the two coordinates but does not remove this negative-product instability.
Hamilton's equations define phase-space velocity . Its divergence is
Thus infinitesimal phase-space volumes are preserved, assuming sufficient differentiability. This is Liouville's theorem; spatial density alone need not be incompressible because the statement concerns the combined coordinate-momentum space.
To match the source's order define . The chain rule and Hamilton's equations then give
Antisymmetry implies , hence , which vanishes for a time-independent Hamiltonian. With the alternative common convention , the same law is ; mixing the two orders would reverse the physical time evolution.
Conservation of probability obeys . Expand the divergence and use incompressibility to obtain , or . This is fine-grained transport for Hamiltonian trajectories without sources or collisions. Coarse graining can obscure this constancy without contradicting it.
For with no explicit time dependence, and . It therefore solves the stationary transport equation. Normalizability and the accessible energy region still have to be checked for a proposed probability distribution.
Axisymmetry supplies conserved in addition to conserved energy. Consequently is a more general stationary solution, since both arguments are constant on every trajectory. Additional independent integrals may permit still more general distributions. This is a sufficient construction, not a claim that every stationary distribution must have exactly these two arguments.

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