In cylindrical coordinates the orthogonal velocity components are r˙, rθ˙, z˙. Their squared magnitudes add, and r˙⋅A=z˙A(r). Thus L=m(r˙2+r2θ˙2+z˙2)/2+qz˙A(r). Taking the curl gives Bθ=−A′(r), consistent with the prescribed field.
Velocity differentiation gives pr=mr˙, pθ=mr2θ˙, pz=mz˙+qA(r). The coordinates θ and z are cyclic, so pθ,pz are conserved. The radial momentum generally changes. In particular the conserved axial canonical momentum differs from the axial mechanical momentum by qA.
The Legendre transform cancels the velocity-linear magnetic term. Expressing velocities in terms of momenta givesThe Hamiltonian is time independent and hence conserved. It equals kinetic energy because a static magnetic field does no work; its dependence on A is through the mechanical momentum combination.
H=2mpr2+2mr2pθ2+2m[pz−qA(r)]2.
The initial condition makes pθ=0 at all times. Accessible radii obey ∣pz−qA(r)∣≤2mH. For q>0 and pz>2mH, monotonicity of A 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 pz/q>0, and are the sorted roots A(r)=(pz±2mH)/q. For example q=−1, A=r, pz=−3, 2mH=1 confines the orbit to 2≤r≤4, but the source's named r1,r2 equations reverse those labels. This is a convention issue, not a failure of confinement.
Expand A(r)=A(r0)+A′(r0)s+O(s2) about qA(r0)=pz. Then pz−qA≃−qA′(r0)s and conservation of energy givesHere Ω=qA′(r0)/m 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 r0, provided the field varies smoothly there.
s˙2+Ω2s2=m2H=Ω2ρ2,ρ=∣Ω∣2H/m,s(t)=ρcos(∣Ω∣t+ϕ).
Use rotating basis vectors with e˙1=Ωe2, e˙2=−Ωe1. The inertial velocity is (x˙1−Ωx2)e1+(x˙2+Ωx1)e2. The two fixed rotating anchors are (0,±a), so the spring lengths are ℓ±=x12+(x2∓a)2. Combining kinetic and elastic energies givesA constant elastic offset has no dynamical effect.
L=2m[(x˙1−Ωx2)2+(x˙2+Ωx1)2]−2k[(ℓ+−l0)2+(ℓ−−l0)2].
Differentiate the quadratic Lagrangian with respect to coordinates and velocities. The equations areThe velocity-cross terms are Coriolis accelerations; moving −Ω2xi 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.
x¨1−2Ωx˙2+(2k′/m−Ω2)x1=0,x¨2+2Ωx˙1+(2k/m−Ω2)x2=0.
Substitution of the exponential ansatz gives the homogeneous amplitude systemA nonzero mode requires zero determinant. Thus (ω12−ω2)(ω22−ω2)=4Ω2ω2 with the stated two effective stiffnesses. The off-diagonal product is positive, which determines the sign on the right.
(ω12−ω2−2iΩω2iΩωω22−ω2)(xˉ1xˉ2)=0.
Put X=ω2 and S=ω12+ω22+4Ω2. Its equation is X2−SX+ω12ω22=0. If both effective stiffnesses are positive, the sum and product of roots are positive and S2−4ω12ω22≥0, so both roots are positive. They can coincide in a degenerate zero-rotation isotropic case; “two” need not mean distinct.
If ω12<0<ω22, 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 (q˙i,p˙i)=(Hpi,−Hqi). Its divergence isThus 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.
∑i(∂qiq˙i+∂pip˙i)=∑i(Hqipi−Hpiqi)=0.
To match the source's order define [a,b]=∑i(apibqi−aqibpi). The chain rule and Hamilton's equations then giveAntisymmetry implies [H,H]=0, hence dH/dt=Ht, which vanishes for a time-independent Hamiltonian. With the alternative common convention {a,b}=∑i(aqibpi−apibqi), the same law is dg/dt=gt+{g,H}; mixing the two orders would reverse the physical time evolution.
dtdg=gt+[H,g].
Conservation of probability obeys ∂tf+∇q,p⋅(fv)=0. Expand the divergence and use incompressibility to obtain ∂tf+v⋅∇q,pf=0, or df/dt=0. This is fine-grained transport for Hamiltonian trajectories without sources or collisions. Coarse graining can obscure this constancy without contradicting it.
For f=F(H) with no explicit time dependence, ∂tf=0 and [H,F(H)]=F′(H)[H,H]=0. 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 pθ in addition to conserved energy. Consequently f=F(H,pθ) 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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