A new stellar mixing process operating below shell convection zones following off-center ignition

TL;DR

This paper uncovers a novel stellar mixing process triggered by unstable composition gradients below convection zones, driven by wave-induced mixing that operates on a dynamical timescale, impacting stellar evolution models.

Contribution

It identifies a new wave-driven mixing mechanism below convection zones in stars with destabilizing composition gradients, expanding understanding beyond traditional thermohaline and overshoot processes.

Findings

Wave fields induce rapid mixing in stable stellar layers.

Mixing occurs on a dynamical timescale, faster than thermohaline processes.

The process is observed across different stellar evolutionary stages.

Abstract

During most stages of stellar evolution the nuclear burning of lighter to heavier elements results in a radial composition profile which is stabilizing against buoyant acceleration, with light material residing above heavier material. However, under some circumstances, such as off-center ignition, the composition profile resulting from nuclear burning can be destabilizing, and characterized by an outwardly increasing mean molecular weight. The potential for instabilities under these circumstances, and the consequences that they may have on stellar structural evolution, remain largely unexplored. In this paper we study the development and evolution of instabilities associated with unstable composition gradients in regions which are initially stable according to linear Schwarzschild and Ledoux criteria. In particular, we explore the mixing taking place under various conditions with multi-dimensional hydrodynamic convection models based on stellar evolutionary calculations of the core helium flash in a 1.25 \Msun star, the core carbon flash in a 9.3\,\Msun star, and of oxygen shell burning in a star with a mass of 23\,\Msun. The results of our simulations reveal a mixing process associated with regions having outwardly increasing mean molecular weight that reside below convection zones. The mixing is not due to overshooting from the convection zone, nor is it due directly to thermohaline mixing which operates on a timescale several orders of magnitude larger than the simulated flows. Instead, the mixing appears to be due to the presence of a wave field induced in the stable layers residing beneath the convection zone which enhances the mixing rate by many orders of magnitude and allows a thermohaline type mixing process to operate on a dynamical, rather than thermal, timescale. We discuss our results in terms of related laboratory phenomena and associated theoretical developments.