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5.3 Parameter File: rhd.par 77 • character bottom_bound: The boundary condition at the bottom of the model is given for instance by character bottom_bound f=A80 b=80 n=’bottom boundary conditions’ & c0=closedbottom transmitting Possible values are: ◦ reflective: closed wall, no gravity, no radiation. Like the velocity field, the magnetic field is mirrored at the boundary. This boundary condition is unphysical, because the magnetic field is an axial vector and it violates the divergence free property of the magnetic field. Therefore, this boundary condition should not be used in MHD simulations. Use closed boundary conditions instead. ◦ constant: open boundary with constant extrapolation of all values, no gravity, no radiation ◦ closed, closedtop: closed wall, can handle gravity, open for outward radiation. Magnetic field lines are orthogonal to the boundary, i.e. the tangential component of the magnetic field vanishes at the boundary. ◦ closedbottom: closed wall, handles gravity, radiation in diffusion approximation. Magnetic field lines are orthogonal to the boundary, i.e. the tangential component of the magnetic field vanishes at the boundary. ◦ periodic: periodic boundaries for hydrodynamics, radiation, and magnetic fields ◦ transmitting: transmitting boundary for hydro and outward radiation. The parameters real c_tchange, real c_tsurf, and real c_hptopfactor have to be specified. Magnetic field lines are orthogonal to the boundary, i.e. the tangential component of the magnetic field vanishes at the boundary. ◦ inoutflow: ”classical” open lower boundary for deep convection, gravity and radiation possible. The parameters real s_inflow, real c_schange, and real c_pchange have to be specified. Magnetic field lines are orthogonal to the boundary, i.e. the tangential component of the magnetic field vanishes at the boundary. ◦ inoutflow2: variant of the open lower boundary condition. The parameters real s_inflow, real c_schange, real c_pchange, and real B1_inflow have to be specified. In simulations of a solar-like star with the MSrad radiation transport module the bottom boundary is typically of type “inoutflow”. A supergiant simulation will have a transmitting lower boundary. • character heat_mode: The mode in which energy is supplied can be adjusted with this parameter. The classical choice is to leave it empty, in which case the mode is chosen from s_inflow (see Sect. 5.3.4) and luminositypervolume (see Sect. 5.3.4). Example: character heat_mode f=A80 b=80 n=’Heating mode’ & c0=’-/bottom_entropy1/bottom_energy1’ bottom_entropy1 Possible values, so far: ◦ : (empty). The classical value. For local models the energy comes through the lower boundary, either by radiation (for a closed bottom boundary closedbottom) or by convection + radiation (for an open bottom boundary inoutflow). ◦ bottom_entropy1: The entropy in the bottom layers (defined as being less than r0_grav above the bottom of the model) is adjusted towards s_inflow on a rate given by c_schange.