CONICET | Buscador de Institutos y Recursos Humanos

Context. White dwarf evolution is essentially a gravothermal cooling process, which, for cool white dwarfs, depends on the treatmentof the outer boundary conditions.Aims. We provide detailed outer boundary conditions that are appropriate to computing the evolution of cool white dwarfs by em-ploying detailed nongray model atmospheres for pure hydrogen composition. We also explore the impact on the white dwarf coolingtimes of different assumptions for energy transfer in the atmosphere of cool white dwarfs.Methods. Detailed nongray model atmospheres were computed by considering nonideal effects in the gas equation of state and chem-ical equilibrium, collision-induced absorption from molecules, and the Lyman α quasi-molecular opacity. We explored the impact ofouter boundary conditions provided by updated model atmospheres on the cooling times of 0.60 and 0.90 M white dwarf sequences.Results. Our results show that the use of detailed outer boundary conditions becomes relevant for effective temperatures lowerthan 5800 K for sequences with 0.60 M and 6100 K with 0.90 M . Detailed model atmospheres predict ages that are up to ≈10%shorter at log(L/L ) = −4 when compared with the ages derived using Eddington-like approximations at τRoss = 2/3. We also analyzethe effects of various assumptions and physical processes that are relevant in the calculation of outer boundary conditions. In particu-lar, we find that the Lyα red wing absorption does not substantially affect the evolution of white dwarfs.Conclusions. White dwarf cooling timescales are sensitive to the surface boundary conditions for T eff < 6000 K. Interestingly enough,nongray effects have few consequences on these cooling times at observable luminosities. In fact, collision-induced absorption pro-cesses, which significantly affect the spectra and colors of old white dwarfs with hydrogen-rich atmospheres, have no noticeableeffects on their cooling rates, except throughout the Rosseland mean opacity.