Abstract

Abstract Based on stellar evolution simulations, we demonstrate that rapidly accreting white dwarfs (WDs) in close binary systems are an astrophysical site for the intermediate neutron-capture process. During recurrent and very strong He-shell flashes in the stable H-burning accretion regime H-rich material enters the He-shell flash convection zone. reactions release enough energy to potentially impact convection, and i process is activated through the reaction. The H-ingestion flash may not cause a split of the convection zone as it was seen in simulations of He-shell flashes in post-AGB and low-Z asymptotic giant branch (AGB) stars. We estimate that for the production of first-peak heavy elements this site can be of similar importance for galactic chemical evolution as the s-process production by low-mass AGB stars. The He-shell flashes result in the expansion and, ultimately, ejection of the accreted and then i-process enriched material, via super-Eddington-luminosity winds or Roche-lobe overflow. The WD models do not retain any significant amount of the accreted mass, with a He retention efficiency of depending on mass and convective boundary mixing assumptions. This makes the evolutionary path of such systems to supernova Ia explosion highly unlikely.

Highlights

  • Trans-iron elements are produced through n-capture nucleosynthesis, such as the slow (s, with a neutron density Nn 1011 cm−3) and the rapid (r, Nn 1020 cm−3) processes (e.g., Kappeler et al 2011; Thielemann et al 2011). Cowan & Rose (1977) proposed that an i process with Nn ∼ 1015 cm−3 intermediate between s and r processes might be triggered when H is mixed into a convective He-burning shell

  • Based on stellar evolution simulations, we demonstrate that rapidly accreting white dwarfs in close binary systems are an astrophysical site for the intermediate neutron-capture process

  • Rate followed by a prolonged period of lower H ingestion, and all of this without split of the He-flash convection zone. If it is confirmed in 3D simulations that no Global Oscillation of Shell H-ingestion (GOSH, Herwig et al 2014) is found in this situation, 1D spherically symmetric simulations of the i-process nucleosynthesis in rapidly accreting WD (RAWD) are probably more realistic compared to the case of postAGB very late thermal pulse (VLTP) models and low-Z AGB models for which 3D stellar hydrodynamics simulations have yet to determine the detailed outcome of the GOSH

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Summary

INTRODUCTION

Trans-iron elements are produced through n-capture nucleosynthesis, such as the slow (s, with a neutron density Nn 1011 cm−3) and the rapid (r, Nn 1020 cm−3) processes (e.g., Kappeler et al 2011; Thielemann et al 2011). Cowan & Rose (1977) proposed that an i process with Nn ∼ 1015 cm−3 intermediate between s and r processes might be triggered when H is mixed into a convective He-burning shell. In the VLTP the He-convection zone reaches into the remaining H-rich atmosphere, which will mix protons into He-burning conditions (Fujimoto 1977; Iben 1982) This mixing triggers i-process nucleosynthesis, and simulations of this situation can reproduce the unusual heavy element i-process fingerprint in Sakurai’s object if mixing predictions from a mixing-length theory (MLT) are modified to reflect possible effects of the inhomogeneous nature of convective-reactive burn in Hingestion events (Herwig et al 2011, 2014). Cassisi et al (1998) reported that ≈ 0.6M WDs that accreted solarcomposition material at rates of 4 · 10−8 and 10−7M /yr would eventually experience He-shell flashes with Hingestion Their simulations ended due to the ensuing numerical difficulties, but Cassisi et al (1998) suggested that those He-shell flashes could lead to substantial additional mass loss as they would cause the WD to evolve back toward the giant branch, just as the VLTP model of Sakurai’s object.

MODEL ASSUMPTIONS AND SIMULATIONS
RESULTS
The multi-cycle He-flash evolution and the He retention efficiency
The i process
CONCLUSION
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