Lecture #9a-- radiative cooling with metals
1) The dominant radiative cooling process in most astrophysical
plasmas at intermediate temperatures (say 1000 to 10,000,000 K)
is when free electrons collide with ions containing bound
electron, excite the bound electrons, who then de-excite and
emit line radiation that escapes the system.
(At lower temperatures, collisional excitation by molecules dominates,
and at higher temperatures, brehmstrahlung and inverse Compton
scattering dominate).
A particular version of this cooling appears in the absence of ionizing
radiation (so not in HII regions), where collisions with free electrons
also control the ionization stage of the gas.
This type of cooling depends trivially on the free electron density (it
is proportional to it, if considered to be a per-particle cooling, due
to the collision rate dependence), so the only nontrivial dependence is
on the electron temperature.
The electron temperature controls
the fraction of free electrons with the necessary energy to excite the
transitions, and it also controls the ionization state of those ions.
So we can define a "radiative cooling function", depending on T, for these
situations, as shown on page 59 in the textbook.
2) The key feature of this cooling function is that it rises with temperature
if T is not too high (below about 200,000 K), as there are more and more
free electrons with the few-eV energies needed to excite the main transitions.
But as you crest over 200,000 K, you begin to strip most ions (except iron)
of all their bound electrons, and the cooling turns over and decreases
with temperature.
This region of falling cooling as T rises is thermally unstable unless the
heating also falls with T, because otherwise higher (or lower)
T leads to less (or more) cooling
and yet higher
(or lower) T. As a result, we rarely find gas in equilibrium between
200,000 K and 1,000,000 K, it is a transitional state (called the "transition
region" in the Sun) where the gas is always on its way to higher or lower
T, depending on its history.