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The STAROX stellar evolution code
Authors:Ian W. Roxburgh
Affiliation:1. Astronomy Unit, Queen Mary, University of London, Mile End Road, London, E1 4NS, UK
2. LESIA, Observatoire de Paris, Meudon, 92195, France
Abstract:This paper describes the STAROX stellar evolution code for the calculation of the evolution of a model of a spherical star. The code calculates a model at time t k , that is the run of pressure, density, temperature, radius, energy flux and related variables on a mesh in mass M i , given the distribution of chemical elements X j (i) at t k and the model at the previous time step t k?1. It then advances the chemical composition to the next time step t k+1 and calculates a new model at time t k+1. This process is iterated to convergence. The model equations are solved by Newton–Raphson relaxation; the chemical equations are solved by an iterative procedure, each element being advanced in turn, and the process repeated to convergence. Convection is modelled by a mixing length model and convective mixing is treated as a diffusive process; chemical overshooting can be incorporated in parametric form. The equation of state is taken from OPAL tables and the opacity from a blend of OPAL and Alexander tables. Nuclear reaction rates are from NACRE but only cover the pp chain and CNO cycle. The atmospheric layers are incorporated in the model by applying the surface boundary condition at small optical depth (τ≈0.001). The mesh in mass M i is usually taken as fixed except that there is a moveable mesh point at the boundary of a convective core. Results are given for models of mass 0.9 and 5.0M with initial composition X=0.7,Z=0.02 evolved to a state where the central hydrogen abundance is X c =0.35, and for a model of mass 2.0M with initial X=0.72,Z=0.02, evolved to X c =0.01 and with core overshooting. In this latter case we compute two models one with and one without a moveable mesh point at the boundary of the convective core to illustrate the importance of having such a moveable mesh point for the determination of the Brunt–Väisälä frequency in the layers outside the core.
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