In the present study we attempt to derive the dust emissivity from the
observed variation in the mid-infrared spectrum. If the dust emissivity
is proportional to
,
where
is the
wavelength and
is a constant, the total flux from a dust
grain
is expected to vary as
with the temperature
T,
where
is the Planck function.
Thus the variation
in the shell flux is directly connected to the emissivity and to the
variation in the dust temperature. In reality, the emissivity is a complicated
function of the wavelength and the emergent dust shell flux is a summation of
the emission from dust grains of different temperatures. To investigate the
actual emissivity of the dust
grains around Z Cyg we adopt a simple dust shell model.
We assume that the dust shell is optically thin and spherically symmetric.
The spectrum of the emergent dust shell flux
is then given by
The temperature of the grains at r is calculated from the radiative
equilibrium condition:
Since the photospheric contribution becomes dominant for wavelengths shorter
than 7 m,
the dust emissivity cannot be estimated from the observations accurately.
The optical properties of the dust grains shorter than 7
m were
calculated for astronomical silicate (Draine & Lee 1984),
assuming spherical
dust grains with a radius of 0.1
m.
The absorptivity in the near-infrared determines the physical size of the dust
shell, but does not affect
the emergent spectrum
because of the assumption of an optically thin dust shell.
For the optical
properties of dust grains at wavelengths longward of 7
m,
we created a set of dust absorption efficiency factors
from the spectrum observed at the first maximum (
)
by changing
the assumed inner dust shell temperature. From Eq. (1) the
relative spectral shape of the
absorption efficiency factor
is derived straightforwardly
from the observed
spectrum owing to the nature of the optically thin dust shell.
The derived absorption
efficiency factor was scaled such that
Q/a = 1.35
m-1 at the
peak around 9.7
m
to agree with that of the astronomical silicate.
This scaling was needed to make the optical properties connect smoothly
at 7
m. The absolute values of the
absorption
coefficient cannot be determined by the present analysis.
By adopting inner dust shell temperature of 400 K, 500 K, 600 K, 700 K, 800 K,
900 K, and 1000 K at the first observation maximum (
),
we have finally obtained a set of 7 dust absorption efficiency factors.
We denoted them as Qi (i=4,...10). To remove the noise originating
from the observed spectrum, we fitted Qi to the spectrum by using an
analytical function.
For spherical grains of
,
the absorption efficiency factor
is given by
With each Qi we fit all the observed spectra with the model, in which
the inner dust shell temperatures
and the inner dust density
are the only free parameters.
The best fit spectra with y0=0.1 and
Q7 for each observed
spectrum are superposed in Fig. 1. Figure 3
shows the parameters of the best fit models for Q4, Q7, and Q10,
where
is normalized to the
maximum at
for each Qi and
is assumed to not
vary from phase to phase. The density
scales as
if
changes
(see Eq. (1)). Although we obtained different
values of
and
for the best fit models with
each Qi, the best fit
spectra appear to not differ from each other.
All of them provide similarly good fits to the
observations. Some examples are
shown in Fig. 4 for y0 = 0.1. The fitted spectra are almost
identical to each other.
Similar results are also obtained for the cases with y0=0 and
y0=0.4.
Therefore, we cannot distinguish between models with the dust emissivities
and density
distributions examined here solely from the quality of the fit.
Dust formation, if it occurs, adds new dust grains to the shell and could lead to a variation in the observed spectrum. However, dust formation is believed to occur mostly at minimum (e.g., Winters et al. 1994) and it is difficult to imagine that dust formation will explain the observed increase in the flux at maximum. The dust velocity near the bottom of the shell is several km s-1for optically thin shells (Habing et al. 1994) and during the interval of the observations the dust grains travel only several 1010 m, which causes a decrease of only a few degrees in the dust temperature even at the bottom of the shell. This hardly affects the emergent spectrum. Furthermore, the motion of the dust is so slow that the decrease in the dust temperature from maximum to minimum cannot be due to removal of hot dust grains even if the observed change at maximum is attributed to the production of newly-formed hot dust grains near the bottom of the dust shell. Therefore we assume that the observed variations originate in the luminosity variation of the central star and that the density distribution does not change over the present observation period. Under these assumptions we investigate whether any of the seven dust emissivities can provide the flux variation compatible with the observations.
We directly use the observed dust
shell flux to estimate the variation in the emergent flux. If the
dust grains stay at the same position and the amount does not change,
the variation in the dust shell flux at each variability phase
can be predicted from the derived
and
compared to the observations. We use the integrated flux of
the observed dust shell from 5 to 45
m as the shell luminosity.
There are some differences in the absolute flux levels between the
SWS and PHT data
(see Appendix A). In the present analysis we use the SWS flux
to have consistency in the comparison of the model with the observations.
Figure 5 shows
the comparison between the observations and the models with Q4, Q7, and
Q10 for y0 = 0.1. In the models
the amount of the dust grains in the shell is fixed for each Qi to provide
the
best match with all the observed spectra. We plot the uncertainties estimated
from the quoted flux errors of the SWS spectra. The differences between the
models are greatest
at the maxima. If we take a high temperature
dust model (Q10), the model
predicts too large a variation from minimum to maximum because it requires
a large change
in the dust temperature to explain the observed variation in the infrared
spectral shape.
In contrast the model of low dust temperature
(Q4) shows too small a
variation between minimum and maximum since a small change in
with Q4 can explain the observed spectral variations.
![]() |
Figure 6:
Reduced ![]() |
To make a quantitative comparison we plot reduced
values
(
/6,
where
and
are the model and observed fluxes, respectively,
is the uncertainty in the flux, and 6 is the number of
degrees of freedom of the fit, the number of the observation epochs (7) minus
the number of the dust amount scaling factor (1))
for each Qi model
in Fig. 6. The emissivity Q7 gives the
smallest
values for
y0=0, 0.1, and 0.4.
The increase in
in the high
temperature models depends on the assumed dust optical properties in the
5-7
m region. We find that
is minimum
for the emissivity
Q7 unless the real dust properties
differ by more than a factor of 3 from those of the assumed
astronomical silicate. Even if we change the 5-7
m absorptivity by
a factor of 10, the minimum is shifted to either Q6 or Q8.
Thus the present results are not sensitive to the absorptivity in 5-7
m.
The models with
the emissivity Q7 provide the most consistent results with the observed
variations in the spectral
shape (
)
and the flux (
).
This can also be inferred from
Fig. 3, where Q7 gives the least variation in
over the variability phase. The model with Q7 predicts a low integrated
flux at the first minimum (
), which marginally agrees
with the observed value, but it agrees with the observed integrated flux
at the rest of the phases within the uncertainties.
The discrepancy between
and 0.79 will be discussed in terms of
possible dust formation near minimum in the next section.
Models with Q6 and Q8 differ
insignificantly from the Q7 model
in
values.
Comparison with the PHT data suggests that the SWS spectrum of the last
observation (
)
may be systematically brighter
by approximately 15-20% relative to the observations at
the other phases (Appendix A).
If we reduce the integrated flux of the last observation
by 20%, then we find that the Q6 model
gives a slightly smaller
value in the integrated flux than the Q7
model.
In the spectrum fit we also find that a change in
by 10%
increases
by a factor of 2, which corresponds
to about 20% change in the predicted flux level.
This changes the minimum in
either to Q6 or Q8.
Therefore, we estimate that
the uncertainty in the determination of the
most likely emissivity is about one division in the emissivity set (100 K)
and conclude that the models with
K at visual maximum provide the best fit to both the
spectral shape and the flux level.
The derived inner dust temperature at maximum is somewhat low compared
to theoretical predictions, but is not significantly different from the
range 800-1000 K suggested by the latest
investigation (Gail & Sedlmayr 1999).
The best fit for Q7 implies a mass-loss rate
(r*/3
,
where
is the dust flow velocity
at the inner shell boundary and
is the gas to dust ratio. If we
take
cm,
,
km s-1,
and D=490 pc (Young 1995), the estimated mass-loss rate
is in fairly good agreement
with the results of the CO observations (
,
Young 1995).
The optical depth at 9.7
m is derived to be 0.08. It is larger than the
previous
estimate (Onaka et al. 1989b) because the present study derives a
higher
,
but confirms that the optically thin approximation
is still valid.
Copyright ESO 2002