Protoplanetary disks are a byproduct of the star formation process. In the
dense mid-plane of these disks, planetesimals and planets are expected to form.
The first step in planet formation is the growth of dust particles from
submicrometer-sized grains to macroscopic mm-sized aggregates. The grain growth
is accompanied by radial drift and vertical segregation of the particles within
the disk. To understand this essential evolutionary step, spatially resolved
multi-wavelength observations as well as photometric data are necessary which
reflect the properties of both disk and dust. We present the first spatially
resolved image obtained with NACO at the VLT in the Lp band of the
near edge-on protoplanetary disk FS Tau B. Based on this new image, a
previously published Hubble image in H band and the spectral energy
distribution from optical to millimeter wavelengths, we derive constraints on
the spatial dust distribution and the progress of grain growth. For this
purpose we perform a disk modeling using the radiative transfer code MC3D.
Radial drift and vertical sedimentation of the dust are not considered. We find
a best-fit model which features a disk extending from 2AU to several
hundreds AU with a moderately decreasing surface density and
Mdisk=2.8×10−2M⊙. The inclination amounts
to i=80∘. Our findings indicate that substantial dust grain growth has
taken place and that grains of a size equal to or larger than 1mm
are present in the disk. In conclusion, the parameters describing the vertical
density distribution are better constrained than those describing the radial
disk structure.Comment: 10 pages, 9 figures, 2 table