Let us consider now the case of an isothermal cloud, for which the
density in the cloud
varies as a function of
the position
in the following way (Binney & Tremaine (1997)):
where is a constant of proportionality. In other
words, because the jet and cloud are maintained in pressure balance,
the pressure acting on the jet is given by:
For this isothermal case, it is easy to verify that the factors
in the expansions for the gravitational potential and the
pressure
as defined by eqs.(17.12)-(17.13)
are given by:
This solution corresponds to that found by
Raga & Cantó (1996) for the case in which no gravity is present,
i.e.
. From the solutions obtained above in eq.(17.14)
and eq.(18.3) it follows that the dimensionless parameter
defined as
:
is a number that parametrises the required solution.
The deflection of jets in isothermal clouds may be important for
interstellar molecular clouds and the jets associated with Herbig-Haro
objects. For this case we can obtain a value for the parameter . If we adopt a particle number density of
, and a temperature
for a cloud with radius
(Hartmann, 1998; Spitzer, 1998), then
The same calculation can be made for the cases of radio jets
interacting with the gas inside a cluster of galaxies. For this case,
typical values are
(Longair, 1992; Longair, 1998).
With these values, the parameter
,
exactly as eq.(18.5).
The fact that jets are formed in various environments such as giant
molecular clouds and the gaseous haloes of clusters of galaxies with the
same values of the dimensionless parameter provides a clue
as to why the jets look the same in such widely different environments.
From its definition, the parameter can be rewritten as
, where
is the mass within a sphere of radius
.
This quantity is roughly the ratio of the gravitational potential energy
from the cloud acting on a fluid element of the jet, to its kinetic energy
at the initial position
. The parameter
is thus
an indicator of how large the deflections due to gravity are going to
affect the trajectory of the jet. The bigger the number
,
the more important the deflection caused by gravity will be. In other
words, when the parameter
the jet becomes ballistic and
bends towards the centre of the cloud. When
the
deflections are dominated by the pressure gradients in the cloud and the
jets bend away from the centre of the cloud.
Fig.(III.3) shows plots for three different values of with initial Mach numbers of
and
. A comparison with a numerical integration of eq.(17.14)
using a fourth-order Runge-Kuta method is also presented in the figures
by dashed lines. This comparison shows that as long as the deflections
are sufficiently small, or as long as the Mach number of the flow in the
jet is sufficiently large, the analytic approximations discussed above
are a good approximation to the exact solution.
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