 
    
    
         
Emission line central stars of planetary nebulae (CSPNe)  often mimic the
spectra of massive WC stars, in spite of having undergone a completely
different evolutionary history, allowing Standard Model analyses to be
performed. One well known example is the low excitation star
CPD-56 8032, showing optical emission features due to 
HeI-II, CII-IV and OII-III. This star has recently 
been studied by Crowther et al. (1996) revealing it to have a dense, 
stratified wind as demonstrated in Fig. 4, with a highly
evolved surface chemistry (Table 1). The wind temperature
of CPD-56
 8032, showing optical emission features due to 
HeI-II, CII-IV and OII-III. This star has recently 
been studied by Crowther et al. (1996) revealing it to have a dense, 
stratified wind as demonstrated in Fig. 4, with a highly
evolved surface chemistry (Table 1). The wind temperature
of CPD-56 8032 obtained from the Standard Model is in excellent 
agreement with that determined independently by De Marco et al. (1996),
validating the assumption of radiative equilibrium.
 8032 obtained from the Standard Model is in excellent 
agreement with that determined independently by De Marco et al. (1996),
validating the assumption of radiative equilibrium.
Overall, Wolf-Rayet type CSPNe (denoted [WC]) show a wider range in
stellar temperatures (20--140kK) than massive WC stars,
with luminosities and mass-loss rates 1--2 dex lower (Hamann 1996).
Chemical abundances are generally comparable with massive
WC stars, although hydrogen may be present in a subset of [WCL] stars.
Studies of [WC]-type CSPNe indicate close physical and chemical 
similarities with PG 1159 stars. A potential evolutionary sequence is  
[WCL] [WCE]
[WCE] PG 1159 stars (Hamann 1996).
PG 1159 stars (Hamann 1996).
   
Figure 4: Theoretical wind properties of the
[WC10] CSPNe CPD-56 8032 from Crowther et al. (1996),
demonstrating the stratification of W-R winds;
 (a)  Theoretical electron temperature distribution 
(kK) as a function of Rosseland optical depth (
 8032 from Crowther et al. (1996),
demonstrating the stratification of W-R winds;
 (a)  Theoretical electron temperature distribution 
(kK) as a function of Rosseland optical depth ( );
 (b) electron density (in cm
);
 (b) electron density (in cm ); 
 (c)
fractional population for carbon;  (d)
velocity distribution (10
); 
 (c)
fractional population for carbon;  (d)
velocity distribution (10 kms
 kms );  (e)
radius scale (in R
);  (e)
radius scale (in R );  (f) line formation regions 
for selected carbon lines
);  (f) line formation regions 
for selected carbon lines