An optically thick medium has optical depth along the relevant path. Photons undergo many interactions before escaping. Radiative diffusion applies under suitable near-isotropy conditions, but a large scattering depth alone does not guarantee thermalization when true absorption is weak.
An optically thin medium has , so attenuation and emission may be expanded to first order in optical depth.
For isotropic emission without significant absorption, integrating the spontaneous photon-production rate along the sightline gives the displayed energy intensity per solid angle. Photon intensity omits the factor . Summing unresolved transitions is necessary before comparing with an observed blended spectral feature.
The absorption coefficient is the fractional reduction of beam intensity per unit path length: when emission and scattering are absent.
A collision or transient molecular pair can possess a dipole even when the isolated molecules do not. The resulting opacity can be important in a dense molecular hydrogen atmosphere. Pair absorption per unit length scales approximately as the product of the two partner number densities, so its mass absorption coefficient is generally density-dependent. It supplies continuum absorption between ordinary spectral lines.
For dust-grain number density and absorption cross-section , the dust optical depth along a path is .
The mass absorption coefficient is absorbing cross-section per unit mass. For identical spherical dust grains of radius , mass , and absorption efficiency , it is .
For isothermal optically thin dust at distance , its measured spectral flux density determines its mass through . Temperature and opacity uncertainty commonly dominate the inferred mass uncertainty.
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Optical depth (or optical thickness) is a measure of how much a medium attenuates (reduces the intensity of) light or other electromagnetic radiation as it travels through that medium. It quantifies the overall effect of absorption and scattering of light along a specific path.