Max Planck Institute for Astronomy - Annual Report 2005
Max Planck Institute for Astronomy - Annual Report 2005
Max Planck Institute for Astronomy - Annual Report 2005
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68 III. Scientific Work<br />
log F /mJy log F /mJy<br />
2<br />
0<br />
-2<br />
-4<br />
2<br />
0<br />
-2<br />
-4<br />
MgSi0 3<br />
Mg 0.6 Fe 0.4 Si0 3<br />
MgFeSi0 4<br />
Mg 1.9 Fe 0.1 Si0 4<br />
C400<br />
C1000<br />
1 1.5 2 2.5 1 1.5 2 2.5<br />
log � 1 1.5 2 2.5<br />
/ �m<br />
Fig. III.2.4: Spectral energy distributions (SEDs) of disks composed<br />
of 1 and 40 µm grains with different grain chemical<br />
compositions, <strong>for</strong> a model resembling the solar system (i.e., the<br />
planets, excluding Mercury and Pluto, and the Kuiper belt as<br />
Once interesting debris disks have been identified by<br />
spItzEr, the next step will be to obtain high-sensitivity<br />
and high-spatial resolution images in scattered light<br />
and/or thermal emission (using, e.g., LBT, JWST, soFIa,<br />
alMa, or saFIr). Of particular interest are the longer<br />
wavelengths, at which observations can constrain the<br />
amount of material farther away from the planet and at<br />
which the emission of the larger dust particles, the ones<br />
that show more prominent structure, dominate. If one<br />
could spatially resolve the disk, the dynamical models<br />
could allow us to locate the perturbing planet. Then we<br />
could compare the in<strong>for</strong>mation derived from the SED<br />
alone with that derived from the resolved image. This is<br />
important to understand the limitations of the characterization<br />
of planetary architectures on the basis of spatially<br />
unresolved debris disks only. In addition, by obtaining<br />
resolved images in one or more wavelengths we can<br />
break the degeneracy expected from the analysis of the<br />
disk SED. In anticipation of these spatially resolved observations,<br />
we have started working on the modeling of<br />
the brightness density distributions arising from debris<br />
disks in the presence of different planetary configurations<br />
(see Fig III.2.6).<br />
log F /mJy log F /mJy<br />
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log � / �m<br />
the source of dust). Top left: Single grain size (40 µm) disk with<br />
planets; Top right: Single grain size (1 µm) disk with planets;<br />
Bottom left: Single grain size (40 µm) disk without planets;<br />
Bottom right: Single grain size (1 µm) disk without planets.<br />
Radiative Transfer Simulations in the Context of<br />
MatIsse Science Case Studies<br />
MatIssE is <strong>for</strong>eseen as a mid-infrared spectro-interferometer<br />
combining the beams of up to four UTs/Ats of<br />
the Very Large Telescope Interferometer (VLTI). MatIssE<br />
will measure closure phase relations and thus offer an<br />
efficient capability <strong>for</strong> image reconstruction. In addition<br />
to the ability to reconstruct images with interferometric<br />
resolution, MatIssE will open three new observing windows<br />
at the VLTI: the L, M, and Q band which all belong<br />
to the mid-infrared domain. Furthermore, the instrument<br />
will offer the possibility to per<strong>for</strong>m simultaneous observations<br />
in separate bands.<br />
MatIssE will also provide several spectroscopic<br />
modes. In summary, MatIssE can be seen as a successor<br />
of MIdI by providing imaging capabilities in the entire<br />
mid-infrared accessible from the ground. The extension<br />
of MatIssE down to 2.7 µm as well as its generalisation<br />
of the use of closure phases make it also a successor of<br />
aMbEr. Thus, in many respects MatIssE will combine and<br />
extend the experience acquired with two first generation<br />
VLTI instruments – MIdI and aMbEr.