In the radius-velocity plane the flux from a thin shell of radius
expanding at velocity
is
expected to form an ellipse which intersects the radius axis at
and the velocity axis at
.
We expect the velocity
to increase with radius and for simplicity we can assume that the
velocity field within the spherical volume is given by a linear form
The MOS energy resolution cannot separate the red and
blue components when they overlap. If we see both the distant red
shifted shell and nearer blue shifted shell in the same beam the
line profile is slightly broadened but the centroid shift is
diminished. The observed Doppler velocities and the best
fit value for
may be slightly biased by this ambiguity, however
most beams appear to be dominated
by either red or blue shifted knots and therefore this bias is
expected to be small. It is fortuitous that the X-ray emission is
distributed in clumps rather than a thin uniform shell since this
enables us to measure the Doppler shift with a modest angular
resolution without red and blue components in the same beam
cancelling each other out.
The left-hand panel of Fig. 11 is a composite image of the
remnant seen in the Si-K, S-K and Fe-K emission lines.
The solid circle indicates
the
arcsec and the dashed circle is
the mean radius of the Si-K and S-K flux
arcsec.
The X-ray image of the remnant provides coordinates x-yin the plane of the sky.
Using the derived radial velocity field within the remnant
we can use the measured Doppler velocities vz to give us
an estimate of
the z coordinate position of the emitting material along the line of
sight thus giving us an x-y-z coordinate
for the emission line flux in each pixel. Using these coordinates we
can reproject the flux into any plane we choose. The right-hand panel
of Fig. 11 shows such
a projection in a plane containing the line-of-sight, North upwards,
observer to the right.
In this reprojection the line emission from Si-K, S-K and Fe-K are reasonably well aligned for the main ring of knots. The reprojection is not perfect because the MOS cameras are unable to resolve components which overlap along the line-of-sight and this produces some ghosting just North of the centre of the remnant. In the plane of the sky Fe-K emission (blue) is clearly visible to the East between the mean radius of the Si+S flux and the shock radius. Similarly in the reprojection Fe-K emission is seen outside the main ring in the North away from the observer. The Si+S knot in the South away from the observer in the reprojection is formed from low surface brighness emission in the South West quadrant of the sky image. The X-ray emitting material is very clumpy within the spherical volume and is indeed surprisingly well characterised by the doughnut shape suggested by Markert et al. (1983). However the distribution is distinctly different to that obtained in similar 3-D studies of the optical knots, Lawrence et al. (1995).
The expansion of Cas A has been measured in various ways; using the proper motion of optical knots (van den Bergh & Kamper 1983; Fesen et al. 1987; Fesen et al. 1988), from the proper motion of radio knots (Anderson & Rudnick 1995), using Doppler shifts of spectral lines from optical knots (Reed et al. 1995; Lawrence et al. 1995), Doppler shift of X-ray line complexes (Markert et al. 1983; Holt et al. 1994; Vink et al. 1996) and the proper motion of X-ray knots (Vink et al. 1999). These methods identify a number of distinct features with different dynamics; Quasi Stationary Flocculi (optical QSF), Slow Radio Knots in the South West (SRK), the main ring of radio knots, the main ring of X-ray knots (continuum + lines 1-2 keV), Fast Moving Knots (optical FMK) and Fast Moving Flocculi (optical FMF).
In proper motion studies it is conventional to express the motion
as an effective expansion time
(years) where R is the
radius of the feature/knot from some chosen centre (arcsec) and
V is the proper motion (arcsec/year).
The deceleration parameter, the ratio of the true age over the expansion
age, can be estimated as
.
There is no need to
deproject the radius or velocity to estimate m. However if
we then wish to estimate a true expansion velocity the R must be
deprojected but still the ratio R/V will remain constant.
Doppler measurements allow some form of deprojection and measured
radii on the sky can be converted to actual radii within the volume
of the remnant as described in the previous section.
Given a radius in arc seconds
and velocity in kms-1
we can calculate an expansion time in years
assuming
a distance in kpc
,
.
Previous authors have used combinations of these measurements
to refine estimates of the age and/or distance. Alternatively
we can adopt some age and distance and compare the radii and expansion
velocities of the various components. The original explosion probably
occured in 1680 (Ashworth 1980) so the age in 2000 is
years.
Distance estimates have varied over the years but recent studies (Reed et al. 1995) have settled on
3.4+0.3-0.1 kpc.
Table 3 gives estimates of the expansion parameters for the
different components. Those marked with an asterisk are from
proper motion studies which estimate the expansion time or
the deceleration parameter directly. For these
the
value has been estimated and the
calculated using
the measured expansion time. From the Doppler measurements we get
a measurement of
and
which are then used to estimate
the expansion time or the deceleration parameter.
Proper motion studies of X-ray emission track the movement of
shock features in the plane of the sky while
X-ray emission line Doppler measurements estimate the velocity of the postshock
plasma
along the line of sight.
The shock velocity
is related to the postshock plasma velocity,
.
The factor
depends on the thermodynamics of the shocked gas
but ranges
between 0.58 for isothermal to 0.75 for
adiabatic conditions, see for example Solinger et al. (1975).
The present X-ray emission line (Xline) results in Table 3
have been calculated from the derived velocity field parameters,
and
using a mean value of
.
The
error quoted reflects the uncertainty in this factor.
The FMF
are at large radii so it is likely that the deprojection correction
is small and the value of 168 arcsec quoted is in fact
the mean radius in the plane of the sky. For the SRK in
the South West sector
and the QSF the values quoted for
are just reasonable
guesses.
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SRK* | ![]() |
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Radio* |
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Xline |
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1 keV* |
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FMK | ![]() |
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FMF* | ![]() |
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Copyright ESO 2002