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On the Equivalence of Equilibrium and Freezing States in Dynamical Systems

C. Evans Hedges

TL;DR

The paper develops a general framework for freezing phase transitions in dynamical systems by linking freezing states to equilibrium states under a fixed potential. It proves that a nonempty set of invariant measures can be realized as the freezing set for some ψ if and only if entropy is constant on that set and the set is an equilibrium set for some φ, with corollaries showing that any ergodic measure is a freezing state for some potential under upper semicontinuity of the entropy map. It further establishes that freezing-favorable potentials are dense in C(X) in the USC setting, while under specification for Z-actions non-freezing potentials form a dense G_δ, and provides insights into the analyticity of the pressure and rapid phase-switching phenomena. These results extend thermodynamic formalism to zero-temperature limits in broad dynamical contexts and furnish constructive tools for engineering freezing behavior across symbolic and smooth systems, with implications for understanding phase transitions and ground-state selection. In particular, the analysis shows that the zero-temperature asymptotics of the modified pressure P_φ(β) are governed by the slant asymptote f(β) = β Max(φ) + h_∞(φ), and that freezing corresponds to achieving this asymptote at some β_0, often accompanied by non-analyticity signaling a phase transition.

Abstract

This paper is concerned with freezing phase transitions in general dynamical systems. A freezing phase transition is one in which, for a given potential $φ$, there exists some inverse temperature $β_0 > 0$ such that for all $α, β> β_0$, the collection of equilibrium states for $αφ$ and $βφ$ coincide. In this sense, below the temperature $1 / β_0$, the system "freezes" on a fixed collection of equilibrium states. We show that for a given invariant measure $μ$, it is no more restrictive that $μ$ is the freezing state for some potential than it is for $μ$ to be the equilibrium state for some potential. In fact, our main result applies to any collection of equilibrium states with the same entropy. In the case where the entropy map $h$ is upper semi-continuous, we show any ergodic measure $μ$ can be obtained as a freezing state for some potential. In this upper semi-continuous setting, we additionally show that the collection of potentials that freeze at a single state is dense in the space of all potentials. However, in the $\Z$ action setting where the dynamical system satisfies specification, the collection of potentials that do not freeze contains a dense $G_δ$.

On the Equivalence of Equilibrium and Freezing States in Dynamical Systems

TL;DR

The paper develops a general framework for freezing phase transitions in dynamical systems by linking freezing states to equilibrium states under a fixed potential. It proves that a nonempty set of invariant measures can be realized as the freezing set for some ψ if and only if entropy is constant on that set and the set is an equilibrium set for some φ, with corollaries showing that any ergodic measure is a freezing state for some potential under upper semicontinuity of the entropy map. It further establishes that freezing-favorable potentials are dense in C(X) in the USC setting, while under specification for Z-actions non-freezing potentials form a dense G_δ, and provides insights into the analyticity of the pressure and rapid phase-switching phenomena. These results extend thermodynamic formalism to zero-temperature limits in broad dynamical contexts and furnish constructive tools for engineering freezing behavior across symbolic and smooth systems, with implications for understanding phase transitions and ground-state selection. In particular, the analysis shows that the zero-temperature asymptotics of the modified pressure P_φ(β) are governed by the slant asymptote f(β) = β Max(φ) + h_∞(φ), and that freezing corresponds to achieving this asymptote at some β_0, often accompanied by non-analyticity signaling a phase transition.

Abstract

This paper is concerned with freezing phase transitions in general dynamical systems. A freezing phase transition is one in which, for a given potential , there exists some inverse temperature such that for all , the collection of equilibrium states for and coincide. In this sense, below the temperature , the system "freezes" on a fixed collection of equilibrium states. We show that for a given invariant measure , it is no more restrictive that is the freezing state for some potential than it is for to be the equilibrium state for some potential. In fact, our main result applies to any collection of equilibrium states with the same entropy. In the case where the entropy map is upper semi-continuous, we show any ergodic measure can be obtained as a freezing state for some potential. In this upper semi-continuous setting, we additionally show that the collection of potentials that freeze at a single state is dense in the space of all potentials. However, in the action setting where the dynamical system satisfies specification, the collection of potentials that do not freeze contains a dense .

Paper Structure

This paper contains 15 sections, 15 theorems, 32 equations.

Key Result

Theorem 1.1

(Corollary 3.17 ruelle) Suppose $h$ is upper semi-continuous and let $\mathcal{E} = \{ \mu_1, \dots, \mu_n \}$ be any finite collection of ergodic measures. Then there exists a potential $\phi \in C(X)$ such that $\mathcal{E}$ is exactly the collection of ergodic equilibrium states for $\phi$.

Theorems & Definitions (27)

  • Theorem 1.1
  • Theorem 1
  • Corollary 2
  • Corollary 3
  • Theorem 4
  • Theorem 5
  • Example 2.1
  • Example 2.2
  • Lemma 3.1
  • proof
  • ...and 17 more