Let us consider the case in which relativistic effects are included
in the collision between a relativistic jet and a stratified high
density region. In order to simplify the problem, the self gravity of
the cloud acting on the jet is ignored. For this case, the relativistic
generalisation of Euler's equation is given by eq.(9.7), in
which and
are the enthalpy per unit volume and the
pressure of a given fluid particle in its proper frame of reference
respectively. The speed of light is
and
is the standard Lorentz factor.
The arguments used to prove the conservation of the angular momentum
of the jet in section §17 can be generalised for the
relativistic case in the following way. The term in brackets in the left
hand side of eq.(9.7) represents the classical force per unit
mass acting on an element of fluid as it moves. By considering steady
flow and because the pressure depends only on the radial coordinate
, vector multiplication of the radius vector
with eq.(9.7) shows that the quantity
is conserved during the
motion of the fluid. This quantity corresponds to the specific angular
momentum in classical mechanics, but is not its relativistic counterpart,
which is given by
. The constancy of
implies that motion is two
dimensional and so eqs.(17.3)-(17.4) are valid in the
relativistic case as well.
Multiplication of eq.(9.7) by the unit tangent vector
for steady adiabatic flow, shows
that the trajectory of the jet is described by Bernoulli's law
(eq.(9.8)):
The line integral is taken from the initial position of a
given fluid particle to its final position. The particle number per unit
proper volume is and we assume that the electrons in the jet are
ultrarelativistic, so that the equation of state is given by
with
being the internal energy density of the plasma.
The requirement that the pressure of the jet equals that of the cloud,
together with the fact that
, makes it
possible to integrate eq.(20.1) giving:
in which
. The sign of
in eq.(20.2) varies
as the jet crosses the cloud. For example, for the ultrarelativistic
case, in which a straight trajectory is expected, it is positive for
, and negative when the inequality
is inverted. A general analytic solution of eq.(20.2) can
be found because, for high relativistic velocities, the third
term on the right hand side of eq.(20.2) is important only
for
. In other words, the pressure
stratification of the cloud can be written as eq.(17.12) with the
substitution
. We can therefore
expand eq.(20.2) about
to obtain a relation like eq.(17.14) but with:
Sergio Mendoza Fri Apr 20, 2001