Abstract

A smoking gun signature for a first-order phase transition with negative speed of sound squared {c}_s^2 is the occurrence of a spinodal instability. In the gauge/gravity duality it corresponds to a Gregory-Laflamme type instability, which can be numerically simulated as the evolution of unstable planar black branes. Making use of holography its dynamics is studied far from and near a critical point with the following results. Near a critical point the interface between cold and hot stable phases, given by its width and surface tension, is found to feature a wider phase separation and a smaller surface tension. Far away from a critical point the formation time of the spinodal instability is reduced. Across softer and harder phase transitions, it is demonstrated that mergers of equilibrated peaks and unstable plateaux lead to the preferred final single phase separated solution. Finally, a new atypical setup with dissipation of a peak into a plateau is discovered. In order to distinguish the inhomogeneous states I propose a new criterium based on the maximum of the transverse pressure at the interface which encodes phase-mixed peaks versus fully phase separated plateaux.

Highlights

  • Develops in four stages: 1) exponential growth of the instability; 2) the reshaping; 3) the merger; 4) the preferred final solution [49, 50]

  • A smoking gun signature for a first-order phase transition with negative speed of sound squared c2s is the occurrence of a spinodal instability

  • Across softer and harder phase transitions, it is demonstrated that mergers of equilibrated peaks and unstable plateaux lead to the preferred final single phase separated solution

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Summary

Criterium for inhomogeneous states

The spinodal instability cools down regions in the unstable energy density, so that they reach the cold stable phase and pushes out the energy density to other regions, which in turn accumulates and may reach the hot stable phase. This results in various inhomogeneous states, which are to be further classified. In what follows I will define the two distinct maxima and minima that form due to the spinodal instability: a peak and a plateau; a gorge and a valley

Definition: peaks versus plateaux and gorges versus valleys
Final stage
Reshaping stage
Merger stage
Characteristics of the interface
Surface tension
Comparison of the formation time
Findings
Discussion
Full Text
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