Scalar-induced gravitational waves including isocurvature perturbations with lattice simulations
Xiang-Xi Zeng
TL;DR
This work investigates scalar-induced gravitational waves (SIGWs) generated by isocurvature perturbations using lattice simulations that handle mixed initial conditions. It validates pure isocurvature results against semi-analytical predictions, reveals that multi-peak structures persist similarly to adiabatic cases, and demonstrates how energy transfer during early matter domination, such as from primordial black holes or solitons, shapes the peak amplitude and slope depending on microphysical properties. The lattice approach provides a robust, nonperturbative framework for predicting SIGW spectra in complex primordial scenarios, with implications for interpreting current and future gravitational-wave observations. Overall, the paper extends SIGW theory beyond adiabatic perturbations and offers practical insights for connecting early-universe microphysics to observable GW signals.
Abstract
Scalar-induced gravitational waves (SIGWs) open a unique window into early-universe physics. While their generation from adiabatic perturbations has been extensively studied, the contribution from isocurvature perturbations remains poorly understood. In this work, we develop a lattice simulation framework to compute the stochastic gravitational wave background from both pure isocurvature and mixed initial conditions. Our numerical results show excellent agreement with semi-analytical predictions in the pure isocurvature case. We further analyze multi-peak structures under general initial conditions and find that they closely match those produced in purely adiabatic scenarios. Additionally, we examine SIGWs in early matter-dominated eras, revealing that the peak amplitude and spectral slope are sensitive to the microphysical properties of the dominant field, such as the primordial black hole mass, abundance, or soliton decay rate. This study establishes lattice simulations as a robust tool for predicting SIGW spectra from complex primordial perturbations, with important implications for interpreting current and future gravitational wave observations.
