Rosseland mean opacity

E46432

Rosseland mean opacity is an average measure of a material’s opacity weighted toward frequencies where radiation is most effectively transported, widely used in stellar and astrophysical radiative transfer calculations.


Statements (48)
Predicate Object
instanceOf astrophysical opacity measure
mean opacity
radiative transfer quantity
appliesTo continuum opacity
line opacity ensembles
assumes diffusion approximation for radiative transfer
local thermodynamic equilibrium
optically thick medium
characteristic emphasizes frequency ranges where radiation diffuses most efficiently
contrastsWith Planck mean opacity weighting by Planck function itself
dependsOn chemical composition
density
frequency-dependent opacity
ionization state
temperature
domain astrophysics
plasma physics
radiative transfer theory
stellar astrophysics
introducedBy Svein Rosseland
introducedIn 20th century
mathematicalDefinition harmonic mean of monochromatic opacity weighted by derivative of Planck function with respect to temperature
namedAfter Svein Rosseland
relatedTo OP opacity project
OPAL opacity project
Planck mean opacity
equation of radiative transfer
flux-mean opacity
monochromatic opacity
radiation pressure
radiative diffusion approximation
radiative energy transport
stellar opacity tables
roleInModels controls radiative energy flux for given temperature gradient
symbol kappa_R
unit square meter per kilogram
usedFor computing radiative temperature gradient in stars
determining convective stability criteria
estimating radiative conductivity
modeling energy transport in stellar interiors
usedIn accretion disk models
astrophysical radiative transfer
interior models of stars
radiation hydrodynamics
stellar atmosphere modeling
stellar evolution models
stellar structure calculations
weightingFunction dB_nu_dT

Referenced by (1)
Subject (surface form when different) Predicate
Radiative Transfer
relatedConcept

Please wait…