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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