Artigo Acesso aberto Revisado por pares

Rosseland and Planck mean opacities for protoplanetary discs

2003; EDP Sciences; Volume: 410; Issue: 2 Linguagem: Inglês

10.1051/0004-6361

ISSN

1432-0746

Autores

D. Semenov, Th. Henning, Ch. Helling, M. Ilgner, E. Sedlmayr,

Tópico(s)

Stellar, planetary, and galactic studies

Resumo

In this paper, we present mean gas and dust opacities relevant to the physical conditions typical of protoplanetary discs. As the principal absorber for temperatures below ~1500 K, we consider spherical and aggregate dust particles of various sizes, chemical structure, and porosity, consisting of ice, organics, troilite, silicates, and iron. For higher temperatures, ions, atoms, molecules, and electrons are included as the main opacity sources. Rosseland and Planck mean opacities are calculated for temperatures between 5 K and K and gas densities ranging from 10-18 g cm-3 to 10-7 g cm-3. The dependence on the adopted model of dust grains is investigated. We compare our results with recent opacity tables and show how different opacity models affect the calculated hydrodynamical structure of accretion discs.

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