Gravitational Wave Mountains: current-carrying domain walls
Anish Ghoshal, Yu Hamada
TL;DR
Domain walls from discrete-symmetry breaking can generate GWs when they annihilate, but current-carrying DWs with trapped fermions introduce a metastable spheron object that imprints a secondary GW peak. The authors develop a semi-analytic framework for such DWs, deriving the spheron radius $R_\text{sph}$ by balancing wall tension against fermion-induced centrifugal energy, and compute the GW spectrum including a fission-driven peak; they also present numerical support for spheron formation. The results show that the spheron-induced peak can be sizable and fall within LISA/ET sensitivity for realistic parameter choices, offering a distinctive signature to distinguish BSM scenarios with DW currents from standard DW backgrounds. This signature enhances the prospects for early-Universe probes of new physics, while motivating lattice simulations and cross-checks with PTA and CMB constraints to map the viable parameter space.
Abstract
Domain wall (DW) networks may have formed in the early universe following the spontaneous breaking of a discrete symmetry. Notably, several particle physics models predict the existence of current-carrying DWs, which can capture and store particles as zero modes on it. In this study, we demonstrate that gravitational waves (GWs) generated by current-carrying DWs with fermionic zeromodes exhibit a novel feature: an additional peak in the GW spectrum resembling mountains, arising from metastable topological remnants, which we term ``spherons.'' This distinct signature could be detectable in upcoming GW observatories such as LISA and ET. The results suggest that DW networks in beyond Standard Model scenarios could emit GW signals that are significantly stronger and with greater detectability than previously expected.
