Three-dimensional simulations of turbulent convective mixing in ONe and CO classical nova explosions
Jordi Casanova, Jordi Jose, Enrique Garcia-Berro, and Steven N. Shore

TL;DR
This paper presents 3D simulations of turbulent mixing in classical nova explosions, comparing the effects of CO and ONe white dwarf substrates on ejecta composition, revealing larger metallicity enhancements with ONe substrates.
Contribution
The study provides the first 3D simulations of mixing at the core-envelope interface for both CO and ONe white dwarfs in nova explosions, highlighting differences in metallicity enrichment.
Findings
ONe-rich substrates produce larger metallicity enhancements.
Kelvin-Helmholtz instabilities facilitate self-enrichment in nova ejecta.
Simulation constraints include resolution and domain size.
Abstract
Classical novae are thermonuclear explosions that take place in the envelopes of accreting white dwarfs in binary systems. The material piles up under degenerate conditions, driving a thermonuclear runaway. The energy released by the suite of nuclear processes operating at the envelope heats the material up to peak temperatures about 100 - 400 MK. During these events, about 10-3 - 10-7 Msun, enriched in CNO and, sometimes, other intermediate-mass elements (e.g., Ne, Na, Mg, Al) are ejected into the interstellar medium. To account for the gross observational properties of classical novae (in particular, the large concentrations of metals spectroscopically inferred in the ejecta), models require mixing between the (solar-like) material transferred from the secondary and the outermost layers (CO- or ONe-rich) of the underlying white dwarf. Recent multidimensional simulations have…
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