Details of the computer code used for solution of the radiative transfer in dusty envelopes can be found in Szczerba et al. (1997). In brief: the frequency-dependent radiative transfer equation is solved for a dust under assumption of spherically-symmetric geometry for its distribution taking into account particle size distribution and quantum heating effects for the very small dust particles.
The modelled source is certainly C-rich (see Omont et al. 1995 and Kwok et al. 1995). Therefore, for modelling of its spectral energy distribution (SED) we assumed that dust is composed of: policyclic aromatic hydrocarbons (PAH) for dust sizes a between 5 and 10Å (see Szczerba et al. (1997) for details concerning PAH properties), amorphous carbon grains (of AC type from Rouleau & Martin 1991) for a>50Å and dust with an opacity obtained from averaging of the absorption efficiences for PAH and AC grains according to the formula:
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The  
m  feature  was approximated by a gaussian with
 parameters   determined   from  modelling  of  IRAS07134+1005
 (centre  wavelength equal to 
m, and width of
 
m)  which has the strongest
 feature  among the known 
m sources. In the case of
 
m band we used the addition of two half-gausians
 with  the same strength and different width. Initial fit was done
 to  IRAS  22272+5435  and  its parameters were: width for short
 wavelength  side  
m, width for
 long  wavelength  side 
m and central
 wavelength  
m  (see  Szczerba et al. 1997). For
 modelling  of  IRAS04296  we  have reduced the strength of this
 feature  by  50%.  Superposition  of the 21 and 
m
 features  was  added to the absorption properties of amorphous carbon
 in order to construct an empirical opacity function (EOF).
In  Fig.7 the best fit obtained from the solution
 of  the  radiative  transfer  problem  including  quantum heating
 effects  for  the PAH grains is shown together with observational
 data  which will be described in detail elsewhere. Note, however,
 that  we  present  also two sets of photometry (from B to M band)
 corrected for interstellar extinction (open symbols)
 according   to   the   average  extinction  law  of  Cardelli  et
 al. (1989),  assuming  that  total  extinction at V is 1.0 or 2.0
 magnitudes  and  plotting  only the smallest and largest value of
 corrected fluxes at given band.
This estimate of the total extinction range can be inferred from the analysis of data presented by Burstein & Heiles (1982).
| parameter | value | 
| 
 | 
6500K | 
| log ( | 
3.92 | 
| d | 5.4kpc | 
| 0.5pc | |
| 12kms-1 | |
| 6.410-4pc | |
| 870K | |
| 4.010-7 | 
|
| 7.0610-3pc | |
| 270K | |
| 1.7010-5 | 
|
| 2.1910-4 | 
|
| a- | 5Å | 
| a+ | 0.25  | 
| p | 3.5 | 
| 575yr | |
| 0.0071 | 
|
The  best  fit to the spectral energy distribution of IRAS04296
 is   shown   by  heavy  solid  line  (see  Table2  for  details
 concerning  parameters of the model). Our modelling procedure was
 such  that  we tried to get fits to SED which fall in between the
 extinction  corrected  fluxes.  In  this  way, we have taken into
 account  not  only the effect of the circumstellar extinction but
 also  of  interstellar  extinction.  The  thin  long-dashed line
 represents  the input energy distribution of the central star for
 logg=0.5   and   
=6500K   according   to   model
 atmosphere  calculations  of  Kurucz (private communication). The
 heavy  short-dashed  line  shows the fit which was obtained with
 the  same  assumptions  but changing the effective temperature of
 the  star  to 6000K. As one can immediately see in the IR range
 of  the  spectrum  the  quality  of  the  fits  are very similar.
 However,  in  the  optical  and  ultraviolet  (UV)  part  of  the
 spectrum  the  fit  assuming  
=6000K  is  not  able to
 explain  extinction  corrected data. In consequence, we are quite
 convinced  that  our  estimation of 
 for IRAS04296 close
 to  6500K  is  reasonable  and,  what  is  even more important,
 agrees  pretty  well with the spectroscopic estimation (6300K).
 Note  that  spectral  type  of  this source was found to be G0 Ia
 from  the low resolution spectrum (Hrivnak 1995) which implies an
 effective  temperature of around 5500K for the star if we asume
 that  the  same relationship applies for post-AGB supergiants as
 for  ``normal''  ones  (see  Schmidt-Kaler 1982). For such a low
 temperature  we  were  not able to fit even the reddenned data in
 the UV.
The  thin  solid  line  in  the wavelength range from about 18 to
 
m represents the model continuum level found after
 solution  of  radiative  transfer equation for dust without using
 the   EOF  parameters  as  in  Tab.2  while  keeping  the  dust
 temperature  (or  probability  distribution  of dust temperature)
 the  same  as  for the case of dust with EOF. Taking into account
 the  estimated continuum level and assuming that 21
m feature
 extends  from  18 to 22 
m we estimate the energy emitted in 21
 
m  band  as  about 5.7 % of the total IR flux (251 
 for
 
's  from 5 to 300 
m assuming a distance to the source
 of  1  kpc).  With the dotted line for wavelengths longer than 18
 
m  we  present  the  fit  which  was obtained using an opacity
 function  with  the  EOF  for only 21 
m component. It is clear
 that  such  fit is not able to explain IRAS photometry at 25 
m.
 Our  recent  ISO observations show that this source is also a
 30
m  emitter. In the forthcoming paper (Szczerba et al. 1998, in
 preparation) we will discuss this finding in detail.