![]() | Annu. Rev. Astron. Astrophys. 1991. 29:
59-88 Copyright © 1991 by Annual Reviews. All rights reserved |
6.3 Active Galactic Nuclei
The integrated light from active galactic nuclei (AGN), primarily QSOs,
will contribute at some level to the diffuse far ultraviolet background.
The intensity of this flux is of considerable interest because
it is generally thought to be the factor that determines the
ionization of intergalactic Lyman clouds and it may photoionize the Galactic halo.
A number of authors have estimated the intensity of this flux
(Jakobsen 1980;
Sargent et al. 1980;
Ikeuchi and Ostriker
1986;
Bechtold et al. 1987;
Martin and Bowyer
1989);
the range of estimates is between 0.1 and 10 CU.
It is clear that the far ultraviolet flux produced by AGN will be too small to be directly disentangled from existing measurements. Future specialized searches may be capable of providing information on this topic.
6.4 Emission from an Intergalactic Medium
Early interest in the cosmic far ultraviolet background was
motivated at least in part by its relevance to the
existence of a cosmologically significant intergalactic
medium (IGM). A high-temperature (> 106 K) IGM would produce
X-ray emission, and a lower-temperature (< 104 K)
medium would produce absorption effects in QSO spectra;
observational constraints on these parameters were interpreted
as ruling out these two scenarios, but the possibility of
an intermediate-temperature IGM remained.
An intermediate-temperature IGM would most likely be detected
by its far ultraviolet emission; the
most likely far ultraviolet radiation would be redshifted Lyman
transitions of HI 1216 Å and HeII
304 Å from an ionized primordial gas
(Field 1959;
Kurt and Sunyaev 1967).
In the early stages of galaxy formation this gas might
be reionized collisionally by the passage of shocks
or by interactions with energetic particles
(Ginzberg and
Ozernoy 1966;
Weymann 1967),
or by photoionization
(Arons and McCray
1970).
The emission spectrum depends upon the details
and time scales of the reionization; in particular,
collisional ionization of the gas produces
much more far ultraviolet radiation than photoionization.
Motivated by these suggestions, a variety of data was searched
for indications of radiation from an intermediate-temperature
IGM (Henry et al. 1978;
Anderson et
al. 1979; and
Jakobsen 1980).
In the 1980s several groups developed more detailed models of far ultraviolet emission from a lukewarm IGM. Jakobsen (1980) showed that special conditions would be required if emission from this source were to contribute substantially (~ 300 CU) to the far ultraviolet background. In particular, collisional ionization and substantial clumping of the IGM would be required, and the thermal input must be carefully proscribed, or direct observational constraints would be violated.
Paresce, McKee, and Bowyer (1980) suggested that fast shocks and photoionization would be the most likely ionization mechanisms and these would produce prompt ionization with substantially less radiation. They examined the case in which the gas is sufficiently highly ionized that the dominant emission lines are produced primarily by recombination. In this scenario, the far ultraviolet emission from the IGM is ~ 10 CU.
Martin, Hurwitz, and
Bowyer (1990)
considered emission from an IGM for a variety of scenarios
and compared their results with improved observational constraints
provided by the X-ray background
(Setti 1990),
the lack of absorption troughs shortward of H Lyman
continuum in the spectra of QSOs
(Gunn and Peterson
1965),
limits on emission in the far ultraviolet background as discussed
in this article, and limits on spatial fluctuations in
the far ultraviolet background
(Martin and Bowyer
1989).
They found that even their most optimistic scenarios,
including collisional ionization and clumping of the IGM,
violated observational constraints for an IGM with
even a relatively low density (15% of the critical density of the universe).
This result is to some extent model-dependent,
but the models employed were sufficiently broad
that either very special and unexpected conditions
occurred in the early universe,
or the far ultraviolet background has at most a component < 10 CUs from
the IGM. A component this small will be difficult to identify.