The recombination time of an hydrogenic ion of atomic number Z
in a thermal plasma is
(Verner & Ferland 1986),
where n is the electron density and
is the temperature
dependent recombination coefficient (e.g. Seaton 1959).
For a relatively cold and dense iron plasma with T=104 K,
s while, for
T=108 K,
s.
Hence, while a cold plasma could have the necessary
recombination rate to ensure the needed fast photon production,
this mechanism would be almost completely damped at higher
temperatures with reasonable values for the electron density.
The main problem with this interpretation is that the temperature
of the plasma absorbing a sizeable fraction of the burst energy
is bound to be large, unless an extreme large density enhances
the radiative cooling rates.
In fact the Compton equilibrium temperature (assuming typical
burst high energy spectra) is of the order of a few times 108 K.
Note that the scattering optical depth is bound to be
in the range 0.1-1 since a sizable fraction of the burst energy must
be absorbed without an excessive smearing of the emission lines.
We conclude that the case of a strong iron line due to repeated photoionization and recombination events during the burst emission faces the problem of a temperature too large to ensure the required fast recombination rate.
The equivalent width (EW) of the line in a solar abundance plasma
has been carefully computed by
Bahcall & Sarazin (1978; see in particular
their Fig. 1) and ranges from several tens of eV at high ( K)
temperatures to
keV at
K.
A very weak line is expected for temperature lower than
K.
For temperatures larger than
K the EW dependence on
temperature can be reasonably approximated as a power law.
Assuming an iron abundance 10 times solar we have:
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(1) |
![]() |
(2) |
In this model the emission line is produced only during the burst event,
but in the observer frame it lasts for R/c.
The observed luminosity of the Compton reflection
component is equal to the
of the absorbed energy, divided by the time R/c:
erg s-1.
The luminosity in the iron line (see e.g.
Matt et al. 1991) is
of this, times the iron abundance in solar units.
Therefore the reflection component
can contribute to the hard X-ray afterglow emission,
and the iron line can have a
luminosity up to
erg s-1, corresponding to fluxes
erg cm-2 s-1 for a z=1 burst.
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