Axiom A

{{Short description|A class of dynamical systems}}

{{About|a property of dynamical systems|the property of arithmetical semigroups|Abstract analytic number theory|the axiom for posets|Baumgartner's axiom}}

In mathematics, Smale's axiom A defines a class of dynamical systems which have been extensively studied and whose dynamics is relatively well understood. A prominent example is the Smale horseshoe map. The term "axiom A" originates with Stephen Smale.{{citation | first=S. | last=Smale | url=https://www.ams.org/bull/1967-73-06/S0002-9904-1967-11798-1/home.html | title=Differentiable Dynamical Systems | journal=Bull. Amer. Math. Soc. | volume=73 | year=1967 | issue=6 | pages=747–817 | zbl=0202.55202 | doi=10.1090/s0002-9904-1967-11798-1| doi-access=free }}Ruelle (1978) p.149 The importance of such systems is demonstrated by the chaotic hypothesis, which states that, 'for all practical purposes', a many-body thermostatted system is approximated by an Anosov system.See [http://www.scholarpedia.org/article/Chaotic_hypothesis Scholarpedia, Chaotic hypothesis]

Definition

Let M be a smooth manifold with a diffeomorphism f: MM. Then f is an axiom A diffeomorphism if

the following two conditions hold:

  1. The nonwandering set of f, Ω(f), is a hyperbolic set and compact.
  2. The set of periodic points of f is dense in Ω(f).

For surfaces, hyperbolicity of the nonwandering set implies the density of periodic points, but this is no longer true in higher dimensions. Nonetheless, axiom A diffeomorphisms are sometimes called hyperbolic diffeomorphisms, because the portion of M where the interesting dynamics occurs, namely, Ω(f), exhibits hyperbolic behavior.

Axiom A diffeomorphisms generalize Morse–Smale systems, which satisfy further restrictions (finitely many periodic points and transversality of stable and unstable submanifolds). Smale horseshoe map is an axiom A diffeomorphism with infinitely many periodic points and positive topological entropy.

Properties

Any Anosov diffeomorphism satisfies axiom A. In this case, the whole manifold M is hyperbolic (although it is an open question whether the non-wandering set Ω(f) constitutes the whole M).

Rufus Bowen showed that the non-wandering set Ω(f) of any axiom A diffeomorphism supports a Markov partition.{{citation | last=Bowen | first=R. | authorlink=Rufus Bowen | title=Markov partitions for axiom A diffeomorphisms | journal=Am. J. Math. | volume=92 | pages=725–747 | year=1970 | issue=3 | zbl=0208.25901 | doi=10.2307/2373370| jstor=2373370 }} Thus the restriction of f to a certain generic subset of Ω(f) is conjugated to a shift of finite type.

The density of the periodic points in the non-wandering set implies its local maximality: there exists an open neighborhood U of Ω(f) such that

: \cap_{n\in \mathbb Z} f^{n} (U)=\Omega(f).

Omega stability

An important property of Axiom A systems is their structural stability against small perturbations.Abraham and Marsden, Foundations of Mechanics (1978) Benjamin/Cummings Publishing, see Section 7.5 That is, trajectories of the perturbed system remain in 1-1 topological correspondence with the unperturbed system. This property is important, in that it shows that Axiom A systems are not exceptional, but are in a sense 'robust'.

More precisely, for every C1-perturbation fε of f, its non-wandering set is formed by two compact, fε-invariant subsets Ω1 and Ω2. The first subset is homeomorphic to Ω(f) via a homeomorphism h which conjugates the restriction of f to Ω(f) with the restriction of fε to Ω1:

: f_\epsilon\circ h(x)=h\circ f(x), \quad \forall x\in \Omega(f).

If Ω2 is empty then h is onto Ω(fε). If this is the case for every perturbation fε then f is called omega stable. A diffeomorphism f is omega stable if and only if it satisfies axiom A and the no-cycle condition (that an orbit, once having left a transitive subset of Ω(f), does not return).

See also

References

{{reflist}}

  • {{cite book | last=Ruelle | first=David | authorlink=David Ruelle | title=Thermodynamic formalism. The mathematical structures of classical equilibrium | series=Encyclopedia of Mathematics and its Applications | volume=5 | location=Reading, Massachusetts | publisher=Addison-Wesley | year=1978 | isbn=0-201-13504-3 | zbl=0401.28016 }}
  • {{cite book | last=Ruelle | first=David | authorlink=David Ruelle | title=Chaotic evolution and strange attractors. The statistical analysis of time series for deterministic nonlinear systems | url=https://archive.org/details/chaoticevolution0000ruel | url-access=registration | others=Notes prepared by Stefano Isola | series=Lezioni Lincee | publisher=Cambridge University Press | year=1989 | isbn=0-521-36830-8 | zbl=0683.58001 }}

Category:Ergodic theory

Category:Diffeomorphisms