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This article has an erratum: [https://doi.org/10.1051/0004-6361/200810401e]


   

Table 5:

Grain properties in the disks1.
Name Midplane Surface
  grains grains
MWC 137 SM $a_{\max}=1$ cm SM $a_{\max}=1~\mu$m
R Mon SM $a_{\max}=1$ cm 86% graphite $^{100\%}_{50\%}$ $a_{\max}=1~\mu$m
MWC 1080 SM $a_{\max}=1$ cm SM $a_{\max}=100~\mu$m
MWC 297 SM $a_{\max}=1$ cm SM $a_{\max}=1~\mu$m
LKHa 215 SM $a_{\max}=1$ cm SM $a_{\max}=100~\mu$m
Z CMa SM $a_{\max}=1$ cm 60% graphite $^{100\%}_{50\%}$ $a_{\max}=1~\mu$m
1 The index of the power-law grain-size distribution is fixed (p=3.5). As a first step, we assumed the standard mixture (SM: 86% silicates/14% graphite) in the midplane and surface layers in all the sources. In the cases of R Mon and Z CMa, we needed to change the dust composition in the surface to fit the SED. The range of allowed values are indicated (small figures) in the Table. See Sect. 5.7 for a detailed discussion of the uncertainties.

Source LaTeX | All tables | In the text

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