Gravitational waves from the sound shell model: direct and inverse phase transitions in the early Universe
Giulio Barni, Simone Blasi, Eric Madge, Miguel Vanvlasselaer
TL;DR
This work analyzes early-Universe first-order phase transitions, contrasting direct (outward) and inverse (inward) hydrodynamics. It combines local thermal equilibrium (LTE) estimates for bubble-wall velocity with the sound-shell model (SSM) to predict the gravitational-wave spectra generated by acoustic modes, accounting for cosmic expansion and the expansion history. A key finding is that, while inverse transitions produce qualitatively different fluid profiles, their GW spectra share strong shape similarities with direct transitions, making discrimination based on spectral shapes challenging unless amplitude information is exploited. The study provides a framework for interpreting stochastic GW backgrounds from inverse PTs and highlights the need for field-fluid simulations to go beyond LTE and improve discriminative power for future GW experiments. Overall, the paper lays out the parameter space, LTE limitations, and GW signatures relevant for distinguishing inverse from direct phase-transition dynamics in the early Universe.
Abstract
Cosmological phase transitions are a frequent phenomenon in particle physics models beyond the Standard Model, and the corresponding gravitational wave signal offers a key probe of new physics in the early Universe. Depending on the underlying microphysics, the transition can exhibit either direct or inverse hydrodynamics, leading to a different phenomenology. Most studies to date have focused on direct transitions, where the cosmic fluid is pushed or dragged by the expanding vacuum bubbles. In contrast, inverse phase transitions are characterized by fluid profiles where the plasma is sucked in by the expanding bubbles. Using the sound shell model, we derive and compare the gravitational wave spectra from sound waves for direct and inverse phase transitions, providing new insights into the potential observable features and the possibility of discriminating among the various fluid solutions in gravitational wave experiments.
