In Fig. 10 we show a few typical examples of how
our model results compare to the observed spectra. In
Fig. .1 we show the observed spectra, the composite of the
continuum and the synthetic MgS feature and the residuals after
subtracting the MgS feature for the complete sample. The fits are very
satisfactory in 50 out of 63 cases. In 25 sources the synthetic
spectra obtained with this very simple model are able to explain the
detailed profile of the "30''
m feature very well. The onset and
range of the feature and even the slight depression between 26-30
m are reproduced by the model. We show a zoomed view of the 30
m region of a few sources that are very well fitted by this
simple model in Fig. 11. Notice the different
apparent shapes of the feature that the model is able to explain.
Volk et al. (2002) discuss the "30''
m feature in IRAS 23304 and
find that they need 2 separate unidentified components in order to
understand the shape of the feature. Figure 11
illustrates that this is not necessarily required.
Examining the complete sample of observed "30'' m features and
the synthetic spectra, we find there are some systematic deviations.
In the sample of C-stars and post-AGB objects there are numerous
examples where the major part of the "30''
m feature is
explained well by our model, but the observed spectra show excess
emission in the 26
m region. The excess is not accounted for using
our CDE fits. The most extreme case is IRAS 19584 but several sources
exhibit the same behaviour. In Sect. 6.1, we
discuss the origin of this discrepancy.
In some cases the synthetic spectra over-predict the flux at the
longest wavelengths. This can be due to the very simplistic method we
have used to estimate the continuum level. As the dust optical depth
decreases with increasing wavelengths, the continuum level estimated
from shorter wavelengths might over-predict the true continuum level.
Note, however, that the discrepancies between the modelled and the
observed spectra in the 26 m region and the 40
m region
cannot be considered completely independently. If we were to weaken
the strength of the MgS feature this would yield a better fit around
45
m but would increase the discrepancy around 26
m. We
also note that MgS produces a weak continuum contribution at 45
m
(see for example Fig. 9). This continuum contribution
is already taken into account when fitting the overall continuum, but
it is still present in the calculated MgS contribution. Therefore, our
model may slightly over-predict the fluxes near 45
m.
As a class, the spectra of most PNe show another systematic
difference. The peak position of the "30'' m feature lies in
general at longer wavelengths than in the post-AGB sources. This is in
accordance with the picture of a slowly expanding and cooling dusty
envelope. We can simulate the same shift in peak position using MgS
grains. However the fits we obtain fail to reproduce the relatively
narrow width of the observed profile. We discuss this deviation of the
profiles in Sect. 6.3.
There are 4 sources in the sample that have a broader "30'' m
feature than can be fit by our simple model. Of these sources,
IRAS 13416 and CD-49 11554 show a slightly flattened and broadened
feature while in the cases of RAFGL 618 and RAFGL 2688 the feature is
very broad with a depression around 30
m. The latter sources are
known to have a very large dust column along the line of sight. Most
likely the feature shape is due to optical depth effects. We discuss
these sources further in Sect. 6.2.
Despite these systematic deviations it is clear that our simple model
is able to explain the profile of the "30'' m feature in good
detail in a very wide range of objects. We conclude that the carrier
of the "30''
m feature in the C-stars and post-AGB objects is
solidly identified with MgS and that the variations in peak
position reflect differences in grain temperature.
![]() |
Figure 11:
Examples of spectra that are very well fitted with MgS in a
single temperature, CDE shape distribution. The black lines
represent the data and the grey line the model. The different
sources have been offset for clarity. The excess around 23 ![]() ![]() |
![]() |
Figure 12:
Some examples of sources with a 26 ![]() |
![]() |
Figure 13:
The effects of optical depth of the profile of the MgS
emission. We show the absorbed MgS emission following
Eqs. (2) and (3)
(grey dashed and solid lines), the profile of the "30'' ![]() |
In Fig. 8, we compare the shape of the "30''
m profile of NGC 7027 with the profiles due to differently shaped
MgS grains. As can be seen an oblate MgS grain with an axes ratio of
10:10:1 exhibits a "30''
m feature which peaks at the right
position. At present we don't know of a physical reason for a
preferred oblate grain shape in PNe, and a broader CDE shape
distribution in the C-stars and post-AGB objects (see also
Sect. 8.4).
The shape of a resonance is also influenced by the presence of a
coating. MgS is very hygroscopic. Under conditions where oxygen is
available in the gas phase MgS can be oxidised and transformed into
MgO (Nuth et al. 1985; Begemann et al. 1994). It is possible
that the MgS is transformed as the central star of the PN heats up and
the UV radiation progressively dissociates the CO molecules yielding
gas phase oxygen. This could lead to MgS grains which are coated by a
thin layer of MgO. We have modelled such grains using the
electrostatic approximation following
Bohren & Huffman (1983, Chap. 5). The result is shown in
Fig. 14, curve 6. As can be seen the "30'' m
resonance is split into two features due to the MgO coating. The
feature at the red wavelength is shifted to longer wavelengths
compared to the pure MgS resonance. However the main feature is on the
blue side of 25
m towards the strong resonance at 18
m in
the pure MgO material, in clear contrast with the observations.
We explore other possible coatings on MgS grains to test their ability
to explain the narrow feature observed in the PNe and the lack of
emission at 26 m. We find that of the composite grains we tested
none give a satisfactory explanation. Mixtures of MgS and FeS have
been discussed in the literature to investigate the nature of the
"30''
m feature (Begemann et al. 1994; Men'shchikov et al. 2001; Henning 2000). Curves 1 and 2 in Fig. 14 show
the result of embedding an FeS core in a mantle of MgS and embedding a
MgS core in a mantle of FeS, respectively. The latter compares most
favourably with the position of the feature in the PNe. However, the
substructure found in the spectrum of the composite grain around
33-37
m is not found in the PNe spectra.
Szczerba et al. (1999) examine grains of amorphous carbon with a
mantle of MgS to compare with the 30 m feature in two post-AGB
objects. We show simulated spectra of such grains and MgS grains
coated with amorphous carbon in Fig. 14, curves 3 and
4 respectively. Curve 3 clearly does not match the observed feature in
the PNe. As can been seen in curve 4 the MgS grains coated with
amorphous carbon absorb less at 26
m than pure MgS and are
therefore a better spectral match to the "30''
m feature of the
PNe. However, the feature to continuum ratio in these grains is about
a factor 2.5 lower than in the pure MgS grains requiring a factor 2.5
more mass in the MgS component in order to explain the observed band
strength. Note also that such grains will still produce a weak feature
at 26 while in some PNe spectra we find no excess at that wavelength
at all.
Lastly, in curve 5 (Fig. 14) we show the effect of water ice on the MgS grains. The effects on the optical properties of a water ice coating are marginal and the profile cannot explain the PNe observations. We conclude that of the composite materials we have experimented with MgS grains coated with amorphous carbon give the best spectral match. However we find no composite grains that match satisfactorily.
We stress that although our model does not reproduce the "30'' m
profile in the PNe in its width it is safe to assume that its
carrier is MgS based. These PNe are believed to be the evolutionary
descendants of the sources which exhibit the MgS feature. The shift
in peak position compared to the post-AGB objects follows naturally
from an expanding and cooling shell. Also, the feature strength for
the PNe is similar to these found in the post-AGBs further
strengthening the physical link between the MgS in the C-stars and the
post-AGBs on one hand and the "30''
m feature in the PNe on the
other (see also Sect. 7).
Copyright ESO 2002