The impact of magnetic fields during tidal disruption events
Simona Pacuraru, Clément Bonnerot, Martin E. Pessah
TL;DR
This work addresses how the magnetic field embedded in a star affects the early evolution of tidal disruption events. By combining global MHD simulations with a semi-analytic model, it maps when magnetic pressure becomes dynamically important and how it alters the debris stream, including rapid transverse widening and a magnetic–tidal equilibrium that can persist during the return to pericentre. A key finding is that if the initial stellar field exceeds roughly 10^4 G, magnetic pressure can magnetically support a substantial portion of the stream within about a year, significantly modifying the returning stream and potentially boosting radio emission from interactions with the ambient medium. The results provide physically motivated initial conditions for later phases of TDEs, with implications for disk formation, MRI development, jet production, and multiwavelength observables such as X-ray and radio signatures.
Abstract
During a tidal disruption event (TDE) the stream debris inherits the magnetic field of the star. As the stream stretches, the magnetic field evolves and can eventually become dynamically important. We study this effect by means of magnetohydrodynamic simulations and a semi-analytic model of the disruption of a main-sequence star by a supermassive black hole. For stellar magnetic fields stronger than $\sim 10^4\,\rm{G}$, magnetic pressure becomes important in a significant fraction of the mass of the stream, leading to a fast increase in its thickness, an effect that may impact its subsequent evolution. We find that this dynamical effect is associated with a phase of transverse equilibrium between magnetic and tidal forces, which causes the stream width to increase with distance to the black hole as $H \propto R^{5/4}$. In the unbound tail, this fast expansion could enhance the radio emission produced by the interaction with the ambient medium, while in the returning stream, it may qualitatively affect the subsequent gas evolution, particularly the gas dynamics and radiative properties of shocks occurring after the stream's return to pericentre. By characterizing the magnetohydrodynamic properties of the stream from disruption to the first return to pericentre, this work provides physically motivated initial conditions for future studies of the later phases of TDEs, accounting for magnetic fields. This will ultimately shed light on the role of magnetic fields in enabling angular momentum transport in the ensuing accretion disk, thereby affecting observable signatures such as X-ray radiation and relativistic outflows.
