Opacity and Radiative Transfer
Bremsstrahlung opacity, Rosseland mean, and optically thin vs thick plasmas
6.1 Introduction to Plasma Opacity
Opacity quantifies how effectively a plasma absorbs or scatters radiation at a given frequency. It determines whether photons can escape freely (optically thin) or are trapped and thermalized (optically thick). The opacity controls the radiative energy balance, spectral emission, and temperature structure of astrophysical and laboratory plasmas.
The absorption coefficient $$\kappa_\nu$$ (units of m^-1) appears in the radiative transfer equation:
where $$I_\nu$$ is the specific intensity, s is the path length, and $$j_\nu$$ is the emission coefficient. The optical depth along a ray is:
A plasma is optically thin when $$\tau_\nu \ll 1$$ (photons escape freely) and optically thick when $$\tau_\nu \gg 1$$ (radiation is trapped and approaches a blackbody spectrum).
6.2 Bremsstrahlung (Free-Free) Opacity
The dominant opacity mechanism in fully ionized plasmas is inverse bremsstrahlung(free-free absorption), where a photon is absorbed by an electron in the Coulomb field of an ion. By Kirchhoff's law, the absorption coefficient is related to the emission coefficient by:
where $$B_\nu(T)$$ is the Planck function. The resulting opacity scales as:
where $$\bar{g}_{ff}$$ is the thermally averaged Gaunt factor (of order unity). The strong temperature dependence T^(-7/2) means that opacity increases dramatically as the plasma cools. The frequency dependence $$\nu^{-2}$$ shows that low-frequency (long-wavelength) radiation is absorbed much more strongly.
Kramers' Opacity Formula
In CGS units, the frequency-integrated free-free opacity (Kramers approximation) is:
6.3 Rosseland Mean Opacity
In optically thick regions, radiation transport is diffusive and can be described by a single frequency-averaged opacity. The appropriate average is the Rosseland mean, which weights by the temperature derivative of the Planck function:
The Rosseland mean is a harmonic average, meaning it is dominated by frequency windows where the opacity is lowest (the most transparent regions). This is physically sensible because radiation preferentially escapes through the most transparent spectral windows.
For pure free-free opacity, the Rosseland mean evaluates to:
Planck Mean Opacity
In contrast, for optically thin emission, the relevant average is the Planck mean:
This is a direct average weighted by the Planck spectrum, emphasizing frequencies where the opacity is highest. The Planck mean always exceeds the Rosseland mean.
6.4 Optically Thin vs Thick Regimes
Optically Thin ($$\tau \ll 1$$)
- Every emitted photon escapes the plasma
- Radiated power depends on volume: $$P \propto n_e^2 \sqrt{T}\,V$$
- Spectrum reflects local emission processes
- Use Planck mean for energy balance
- Most fusion and space plasmas
Optically Thick ($$\tau \gg 1$$)
- Radiation is reabsorbed and thermalized
- Radiative flux depends on surface area: $$F = \sigma T^4$$
- Interior approaches LTE (blackbody spectrum)
- Use Rosseland mean for diffusive transport
- Stellar interiors, dense Z-pinches
The transition between regimes depends on density, temperature, and plasma size. Radiative cooling is most effective in the optically thin limit, where increasing density rapidly increases radiation losses. In the optically thick limit, radiation is trapped and the cooling rate saturates at the blackbody surface flux.
6.5 Computational Example
The following code computes and plots the bremsstrahlung emission spectrum and evaluates the Rosseland mean opacity as a function of temperature.
Bremsstrahlung Spectrum and Rosseland Mean Opacity
PythonClick Run to execute the Python code
Code will be executed with Python 3 on the server