Tidal disruption events with SPH-EXA: resolving the return of the stream

TL;DR

This study uses high-resolution GPU-based simulations to investigate tidal disruption events, revealing that stream-stream collisions, not shock dissipation at pericentre, likely mediate debris circularisation.

Contribution

The paper presents the highest-resolution SPH simulations of TDEs, challenging previous assumptions about shock-induced dissipation during stream return.

Findings

Significant debris spreading diminishes at higher resolutions.

No change in stream widths observed at 10^10 particles.

Stream-stream collisions are the primary circularisation mechanism.

Abstract

In a tidal disruption event (TDE), a star is disrupted by the tidal field of a massive black hole, creating a debris stream that returns to the black hole, forms an accretion flow, and powers a luminous flare. Over the last few decades, several numerical studies have concluded that shock-induced dissipation occurs as the stream returns to pericentre (i.e., pre-self-intersection), resulting in efficient circularisation of the debris. However, the efficacy of these shocks is the subject of intense debate. We present high-resolution simulations (up to 10^10 particles) of the disruption of a solar-like star by a 10^6M_sun black hole with the new, GPU-based, smoothed-particle hydrodynamics code SPH-EXA, including the relativistic apsidal precession of the stellar debris orbits; our simulations run from initial disruption to the moment of stream self-intersection. With 10^8 particles - corresponding to the highest-resolution SPH simulations of TDEs in the pre-existing literature - we find significant, in-plane spreading of the debris as the stream returns through pericenter, in line with previous works that suggested this is a significant source of dissipation and luminous emission. However, with increasing resolution this effect is dramatically diminished, and with 10^10 particles there is effectively no change between the incoming and the outgoing stream widths. Our results demonstrate that the paradigm of significant dissipation of kinetic energy during pericentre passage is incorrect, and instead it is likely that debris circularisation is mediated by the originally proposed, stream-stream collision scenario.