Hydrodynamical shear mixing in subsonic boundary layers and its role in the thermonuclear explosion of classical novae
Marco Bellomo, Steven N. Shore, Jordi Jos\'e

TL;DR
This study investigates how hydrodynamical shear mixing in the boundary layer of accreting white dwarfs influences the thermonuclear runaway in classical novae, revealing significant impacts on explosion timing, ejecta properties, and element yields.
Contribution
It introduces a new two-dimensional hydrodynamical simulation of shear mixing at the boundary layer and integrates it into nova models, showing altered explosion characteristics.
Findings
Shorter time to peak temperature in nova explosions.
Greater ejected mass and higher ejecta velocity.
Reduced 7Li production by about an order of magnitude.
Abstract
The transition zone between the white dwarf (WD) envelope and a circumstellar accretion disk in classical novae, the boundary layer, is a region of strong dissipation and intense vorticity. In this strongly sheared layer, the hydrogen-rich accreted gas is expected to mix with the underlying WD outermost layers so the conditions for the onset of the thermonuclear runaway (TNR) in classical nova will be different from the the standard treatment of the onset and subsequent mixing. We applied the critical layer instability (CLI) to the boundary between a disk-accreted H/He zone and the C/O - or O/Ne - rich outer layers of a mass-accreting WD in a cataclysmic binary and then used the resulting structure as input to one-dimensional nuclear-hydrodynamic simulations of the nova outburst. We simulated the subsonic mixing process in two dimensions for conditions appropriate for the inner disk and…
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Taxonomy
TopicsLaser-Plasma Interactions and Diagnostics · Astrophysical Phenomena and Observations · Gamma-ray bursts and supernovae
