In the previous analysis, the problem of a collision of a plane
parallel shock wave with a high density cloud bounded by two plane
parallel tangential discontinuities has been discussed. Radiation losses,
magnetic fields and self gravity of the cloud were neglected. General
analytic solutions were found for the simple case in which the ratio of
the environment's density to that of the cloud's density is a quantity
of the first order.
When the shock collides with the boundary of the cloud, a discontinuity
in the initial conditions is produced. This splits the incoming shock
into two shock waves: one which penetrates the cloud and one which is
reflected back to the external medium. When the transmitted shock into
the cloud reaches the opposite boundary, another discontinuity in the
initial conditions is produced, causing the transmission of a shock
wave to the external medium and the reflection of a rarefaction wave
from the point of collision.
Figure V.5:
Variation of the pressure and density
(with respect to the initial pressure and density
of the environment) as a function of position
(normalised to the initial width of the cloud
) and dimensionless time (in units of the
time
-where is the speed of sound in
the external medium). Dashed lines represent shock waves
(S), dot-dashed lines are tangential discontinuities (T),
which are boundaries of the cloud, and short-long dashed
lines represent weak discontinuities (W), which bound a
rarefaction wave. The system of reference was chosen so
that gas far away to the right of the diagram is at rest. The
diagram shows the case for which
,
and the polytropic indices correspond to a monoatomic gas.
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Figure V.6:
Variation of the width of the cloud in units of its original
size as a function of the dimensionless quantity
. Where represents the sound
speed of the gas for the external environment and
the time. The curve was produced under the assumption
that
. The gas was considered
to be monoatomic.
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Sergio Mendoza Fri Apr 20, 2001