Table 5: Results of our $\chi ^2$-fit presented in Fig. 7. The used method is described in Schegerer et al. (2006) in detail. The underlying continuum is estimated by a single blackbody function with the temperature T. ``RMC'' stands for relative mass contribution, ``am.-sma.'' for amorphous, $0.1\ {\rm\mu m}$-small, ``am.-la.'' for amorphous, $1.5\ {\rm\mu m}$-large and ``crys.'' for crystalline silicate dust grains. The crystalline component includes small and large silicate species: forsterite, enstatite, and quartz. See text for further discussion.

\begin{displaymath}\begin{tabular}{lcccr}\hline\hline
& Baseline length & Resol...
... & & & $T$ & $(722 \pm 9)\ {\rm K}$ \\
\hline
\end{tabular} \end{displaymath}


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