Are such masses compatible with dust made from SN material?
In DLC99, we have argued that the dust observed from Cas A was silicate dust
made from SN material; the layer in the SN where silicate components
(Si, Mg and O) are present, was identified in Fig. 2 of DLC99.
If we take the relative abundance of elements in the "silicate layer''
(Woosley & Weaver 1995), we can evaluate the mass ratio of the different
dust species relatively to the gas. Assuming that the dust formation
efficiency is 100%, then almost all the magnesium and part
of the silicon is locked in MgSiO3 dust grains; the remaining silicon
is locked in SiO2 dust grains; all the aluminium is locked in
Al2O3 dust grains, and the remaining gas is almost entirely
made of oxygen. In these conditions,
,
and
.
The size of the cooling region, and the density derived from CFHT observations
allow to calculate the mass of gas available in the cooling area.
This region is very thin; SD95 obtained a cooling length,
,
of 21011cm for an initial oxygen density of
1.2103cm-3 (here the oxygen density has been taken
equal to
/2 according to the degree of oxygen ionization
calculated in SD95 in the ionization area). Then the mass of gas available in the
cooling region of a
single knot is 1.310-7
;
consequently, if we consider a dust formation efficiency of 100%, we obtain
= 5.310-8
,
= 1.810-8
and
= 4.310-9
.
Thus the observed and potentially available dust masses are compatible.
Comparing the observed dust masses and the calculated maximum dust mass produced from SN material in a knot, we can evaluate the dust "formation'' efficiency. When the SWS aperture contains many knots, a map obtained at 9.77m with ISOCAM using the smallest pixel field of view
of 1.5
,
shows that the hot component originates mainly (50%) from the bright knot of the SWS aperture of
Fig. 1. For this knot, we can derive an estimate of dust formation efficiency of
= 7.4%,
= 8.6% and
= 13%.
Given the simplifications in the model and the
uncertainties in the parameters of the region (a factor 2 of error on the initial
density leads to a factor 2 of error on the efficiency), we can just state that the
efficiency is of the order of 10%. Note that the observed
/
and
/
ratios are well predicted by the model.
The dust mass in the region behind the cooling area
is difficult to determine. An upper limit to the dust mass can be obtained by
considering the total dust mass in a knot. From the gas to dust mass ratio (DLC99)
and the density previously discussed,
we can derive a total dust mass of
= 4.210-4
,
= 1.510-4
and
= 3.410-5
,
in the brightest knot in the SWS aperture.
If we assume, as for the hot component, that half of the cold dust is located into this knot, the observed cold component from the knot represents about 14% of the maximum MgSiO3 and SiO2 dust masses. We are in the uncomfortable situation that the efficiency deduced for the cold dust is somewhat higher than that deduced from the hot component. The assumption that half of the observed cold dust is present in a bright knot, which cannot be tested because of the poor angular resolution of the SWS instrument, is questionable. Indeed the cold component emission lasts longer than the hot component emission, just because of the rapid cooling of region where the dust hot component is emitted and the rapid propagation of the shock inside the knot. Then it is quite possible that several knots with no or little hot dust emission are present in the SWS beam; this would explain why we
observe so much dust in the cold component.
Note that the Al2O3 cold component mass is only 5% of the total expected
dust mass. The origin of such a large depletion compared to MgSiO3 or
SiO2 may be linked to the small size (10 Å) of the grains, which are
more easily destroyed by sputtering effects in the cooling area than
the 70 Å sized particles.
One consequence of the model presented here is the temporal correlation
between the optical emission at the shock and the hot dust emission. We also predict an
increase with time of the IR emission from the cold dust component.
Monitoring the knots both in the IR and the optical on the time scale of the
knot optical lifetime (about 30 years) should help qualifying the model
presented here. High angular resolution at 20m are also needed to assess if there are indeed knots emitting mostly at 20
m, with faint counterparts in the optical or at 10
m.
Acknowledgements
We thanks A. Jones and J.-P. Chièze for enlightening discussions on shocks and their effects, and D. Péquignot for discussions on the optical emission.
Copyright ESO 2001