Entering the Wind Roche Lobe Overflow realm in Symbiotic Systems
R. F. Maldonado, J. A. Toalá, E. Tejeda, J. B. Rodríguez-González
TL;DR
The paper combines stellar evolution with N-body dynamics to study wind accretion, WRLO, drag, and tidal effects in compact symbiotic binaries (2–7 AU). It shows that systems can transition between standard wind accretion and WRLO during high donor mass-loss phases, and that wind drag and tides drive progressively more compact orbits, with tidal decay best matching observed compact systems. Only a minority of cases reach the Chandrasekhar limit, primarily when WRLO operates in high-mass WD and donor configurations; many systems terminate at Roche-lobe overflow, which is not hydrodynamically modeled here. The results underscore tidal forces as a key ingredient in the evolution of compact symbiotics and suggest that observations reflect ongoing tidal orbital decay in these binaries.
Abstract
We present a suite of dynamical simulations designed to explore the orbital and accretion properties of compact (2$-$7 AU) symbiotic systems, focusing on wind accretion, drag forces, and tidal interactions. Using three levels of physical complexity, we model systems of accreting white dwarfs (WDs) with masses of 0.7, 1.0, and 1.2 M$_\odot$ orbiting evolving Solar-like stars with 1, 2, and 3 M$_\odot$. We show that systems alternate between standard wind accretion and Wind Roche Lobe Overflow (WRLO) regimes during periods of high mass-loss rate experienced by the donor star (the peak of red giant phase and/or thermal pulses). For some configurations, the standard wind accretion has mass accretion efficiencies similar to those obtained by WRLO regime. Tidal forces play a key role in compact systems, leading to orbital shrinkage and enhanced accretion efficiency. We find that systems with high-mass WDs ($\geq 1$ M$_\odot$) and massive donors (2$-$3 M$_\odot$) are the only ones to reach the Chandrasekhar limit. Interestingly, the majority of our simulations reach the Roche lobe overflow condition that is not further simulated given the need of more complex hydrodynamical simulations. Our analysis shows that increasing physical realism, by including drag and tides, systematically leads to more compact final orbital configurations. Comparison with compact known symbiotic systems seems to suggest that they are very likely experiencing orbital decay produced by tidal forces.
