Arnold diffusion for generic nearly integrable systems
In plain words
Arnold conjectured that in typical nearly regular systems with three or more degrees of freedom, some orbits drift by a finite amount no matter how small the perturbation. This is proven only in a weaker sense of typical, or for low numbers of degrees of freedom.
Precise statement
$H = h(I) + \varepsilon f(\theta, I)$, (theta, I) in T^n x R^n, h strictly convex, $n \ge 3$. Prove that for generic f (residual in $C^r$, r large; separately, for an open set of analytic f) and all small $\varepsilon > 0$ there are orbits with $\mid I(T) - I(0) \mid \ge c$ with c independent of $\varepsilon$. Answer: a proof for every $n \ge 3$.
What would settle it
A proof valid for arbitrary n with residual (or analytic open) genericity.
Status in the literature
Proven for two and a half degrees of freedom for cusp-residual $C^r$ perturbations (Kaloshin and Zhang, Annals of Mathematics Studies 2020; Cheng); arbitrary n in a weaker cusp-residual sense (Bernard, Kaloshin and Zhang, Acta Mathematica 2016); genuinely residual or analytic perturbations remain open.
See also
- Related KAM tori for the planetary N-body problem with actual masses
- Related Mechanism and duration of the disruption thermal quench
- Related Rate of chaotic action diffusion in weakly nonlinear 4D maps
- Related Optimal diffusion time compared with the Nekhoroshev stability bound
- Related Generic Lyapunov instability of elliptic equilibria in many degrees of freedom