4.6 Article

Radiative transfer and the energy equation in SPH simulations of star formation

Journal

ASTRONOMY & ASTROPHYSICS
Volume 475, Issue 1, Pages 37-49

Publisher

EDP SCIENCES S A
DOI: 10.1051/0004-6361:20077373

Keywords

stars : formation; methods : numerical; radiative transfer; hydrodynamics; ISM : clouds

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Aims. We introduce and test a new and highly efficient method for treating the thermal and radiative effects influencing the energy equation in SPH simulations of star formation. Methods. The method uses the density, temperature and gravitational potential of each particle to estimate a mean optical depth, which then regulates the particle's heating and cooling. The method captures -at minimal computational cost -the effects of (i) the rotational and vibrational degrees of freedom of H(2); (ii) H 2 dissociation and Ho ionisation; (iii) opacity changes due to ice mantle melting, sublimation of dust, molecular lines, H(-), bound-free and free-free processes and electron scattering; (iv) external irradiation; and (v) thermal inertia. Results. We use the new method to simulate the collapse of a 1 M(circle dot) cloud of initially uniform density and temperature. At first, the collapse proceeds almost isothermally (T proportional to rho(0.08); cf. Larson 2005, MNRAS, 359, 211). The cloud starts heating fast when the optical depth to the cloud centre reaches unity (rho(C) similar to 7 x 10(-13) g cm(-3)). The first core forms at. rho(C) similar to 4 x 10(-9) g cm(-3) and steadily increases in mass. When the temperature at the centre reaches T(C) similar to 2000 K, molecular hydrogen starts to dissociate and the second collapse begins, leading to the formation of the second (protostellar) core. The results mimic closely the detailed calculations of Masunaga & Inutsuka (2000, ApJ, 531, 350). We also simulate (i) the collapse of a 1.2 M(circle dot) cloud, which initially has uniform density and temperature, (ii) the collapse of a 1.2 M(circle dot) rotating cloud, with an m = 2 density perturbation and uniform initial temperature, and (iii) the smoothing of temperature fluctuations in a static, uniform density sphere. In all these tests the new algorithm reproduces the results of previous authors and/ or known analytic solutions. The computational cost is comparable to a standard SPH simulation with a simple barotropic equation of state. The method is easy to implement, can be applied to both particle-and grid-based codes, and handles optical depths 0 < tau less than or similar to 10(11).

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