Astron. Astrophys. 329, 845-852 (1998)
4. Matter distribution
Here we discuss the matter distribution of both the uniform and
cloudy medium through which the jet propagates as well the density and
characteristic size of the clouds. The density distribution of
extensive halos around giant elliptical galaxies follows a general law
of the type
![[EQUATION]](img72.gif)
where and is the
density at the galactic center (Forman et al., 1985). If we put
kpc for the characteristic radius and
cm-3, then
will represent the density distribution around an extended source.
This distribution should be appropriate to study the propagation of
the jet outside the galactic central regions. It has been used in a
simplified form by Fanti et al. (1995) in the case of kiloparsec-sized
steep-spectrum sources. However, in the case of compact sources, the
distances from the central object are much smaller, of the order of
tens of parsec and one expects the density to be higher. Therefore, we
add a second, short-scale height component, which enables us to
describe the motion of the jet near the galactic center. In this case
one would take cm-3 and a
characteristic radius pc. Therefore the
density distribution has the form,
![[EQUATION]](img79.gif)
Consider now a cloudy medium surrounding the central object. Not
much information exists on the distribution and structure of the
clouds. Assuming that the galaxy has suffered an increase in the gas
density due to an interaction or merger with a gas-rich companion, we
suppose that this gas will form clouds that will be distributed around
the central object up to an outer radius . An
inner boundary of the cloud distribution must
also exist if the individual clouds are to be stable against tidal
forces. If, for instance, the mass of the central object is of the
order of the lower limit of
is pc otherwise the
density of the clouds will be much greater than
cm-3.
We shall suppose that the clouds' contribution to the mean density
is also given by the general law (8) but with a much smaller value of
, around pc and
cm-3. We shall call this density
. It is given by
![[EQUATION]](img89.gif)
and
![[EQUATION]](img90.gif)
The outer radius of the cloud region can
only be estimated roughly and should not be much larger than the
galaxy central region. One constraint to is the
total mass present inside the cloudy region. If we take this to be
then for the value of
above one must have in the range 200-500 pc. We
therefore take a characteristic value pc as a
lower limit.
The number of clouds per unit length and the
internal density of the clouds should be such
that the mean density of the ambient medium is
achieved. The average number of clouds per unit
length is then given by
![[EQUATION]](img93.gif)
Since the linear density always appears
multiplied by we also give the expression
![[EQUATION]](img94.gif)
where is the particle number density of the
cloud. We assume that depends on the distance
from the central object. For instance, in the case of dense,
self-gravitating clouds, if they were to be stable against tidal
disruption, one would have . Since other factors
also may come into play, we generalize this and use the following
parametrization
![[EQUATION]](img96.gif)
where is a free parameter in the range 0-3.
The value of depends on the mass of the central
object and of the radius of the inner boundary
of the cloud distribution and it is given
by
![[EQUATION]](img100.gif)
This expression ensure that the cloud will always withstand tidal
forces at .
Finally, the radius of the clouds should not
be constant so that we allow for a linear increasing with the distance
R, that is,
![[EQUATION]](img102.gif)
© European Southern Observatory (ESO) 1998
Online publication: December 16, 1997
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