Issue |
A&A
Volume 691, November 2024
|
|
---|---|---|
Article Number | A148 | |
Number of page(s) | 17 | |
Section | Planets and planetary systems | |
DOI | https://doi.org/10.1051/0004-6361/202451589 | |
Published online | 08 November 2024 |
Dust mineralogy and variability of the inner PDS 70 disk
Insights from JWST/MIRI MRS and Spitzer IRS observations
1
Department of Astrophysics/IMAPP, Radboud University,
PO Box 9010,
6500
GL Nijmegen,
The Netherlands
2
SRON Netherlands Institute for Space Research,
Niels Bohrweg 4,
2333
CA
Leiden,
The Netherlands
3
Space Research Institute, Austrian Academy of Sciences,
Schmiedlstrasse 6,
8042
Graz,
Austria
4
Kapteyn Astronomical Institute,
Rijksuniversiteit Groningen, Postbus 800,
9700AV
Groningen,
The Netherlands
5
Institute for Theoretical Physics and Computational Physics, Graz University of Technology,
Petersgasse 16,
8010
Graz,
Austria
6
RIKEN Cluster for Pioneering Research,
2-1 Hirosawa, Wako-shi,
Saitama
351-0198,
Japan
7
Max-Planck-Institut für Astronomie (MPIA),
Königstuhl 17,
69117
Heidelberg,
Germany
8
Institute of Astronomy, KU Leuven,
Celestijnenlaan 200D,
3001
Leuven,
Belgium
9
STAR Institute, Université de Liège,
Allée du Six Août 19c,
4000
Liège,
Belgium
10
Centro de Astrobiología (CAB), CSIC-INTA, ESAC Campus,
Camino Bajo del Castillo s/n,
28692
Villanueva de la Cañada, Madrid,
Spain
11
Leiden Observatory, Leiden University,
PO Box 9513,
2300
RA
Leiden,
the Netherlands
12
Max-Planck Institut für Extraterrestrische Physik (MPE),
Giessenbachstr. 1,
85748,
Garching,
Germany
13
Dept. of Astrophysics, University of Vienna,
Türkenschanzstr. 17,
1180
Vienna,
Austria
14
ETH Zürich, Institute for Particle Physics and Astrophysics,
Wolfgang-Pauli-Str. 27,
8093
Zürich,
Switzerland
15
Université Paris-Saclay, Université Paris Cité, CEA, CNRS, AIM,
91191
Gif-sur-Yvette,
France
16
SRON Netherlands Institute for Space Research,
PO Box 800,
9700
AV,
Groningen,
The Netherlands
17
Université Paris-Saclay, CNRS, Institut d’Astrophysique Spatiale,
91405
Orsay,
France
★ Corresponding author; hyerin.jang@astro.ru.nl
Received:
20
July
2024
Accepted:
28
August
2024
Context. The inner disk of the young star PDS 70 may be a site of rocky planet formation, with two giant planets detected further out. Recently, James Webb Space Telescope/Mid-Infrared Instrument (JWST/MIRI) Medium-Resolution Spectrometer (MRS) observations have revealed the presence of warm water vapour in the inner disk. Solids in the inner disk may inform us about the origin of this inner disk water and nature of the dust in the rocky planet-forming regions of the disk.
Aims. We aim to constrain the chemical composition, lattice structure, and grain sizes of small silicate grains in the inner disk of PDS 70, observed both in JWST/MIRI MRS and the Spitzer Infrared Spectrograph (Spitzer IRS).
Methods. We used a dust fitting model, called DuCK, based on a two-layer disk model considering three different sets of dust opacities. We used Gaussian random field and distribution of hollow spheres models to obtain two sets of dust opacities using the optical constants of cosmic dust analogs derived from laboratory-based measurements. These sets take into account the grain sizes as well as their shapes. The third set of opacities was obtained from the experimentally measured transmission spectra from aerosol spectroscopy. We used stoichiometric amorphous silicates, forsterite, and enstatite in our analysis. We also studied the iron content of crystalline olivine using the resonance at 23–24 μm and tested the presence of fayalite. Both iron-rich and magnesium-rich amorphous silicate dust species were also employed to fit the observed spectra.
Results. The Gaussian random field opacity set agrees well with the observed spectrum, better than the other two opacity sets. In both MIRI and Spitzer spectra, amorphous silicates are the dominant dust species. Crystalline silicates are dominated by iron-poor olivine. The 23–24 μm olivine band peaks at 23.44 μm for the MIRI spectrum and 23.47 μm for the Spitzer spectrum, representing around or less than 10% of iron content in the crystalline silicate. In all of the models, we do not find strong evidence for enstatite. Moreover, the silicate band in the MIRI spectrum indicates larger grain sizes (a few microns up to 5 μm) than the Spitzer spectrum (0.1–1 μm), indicating a time-variable small grain reservoir.
Conclusions. The inner PDS 70 disk is dominated by a variable reservoir of warm (T~350–500 K) amorphous silicates, with ~15% of forsterite in mass fraction. The 10μm and 18μm amorphous silicate bands are very prominent, indicating that most emission originates from optically thin dust. We suggest that the small grains detected in the PDS 70 inner disk are likely transported inward from the outer disk as a result of filtration by the pressure bump associated with the gap and fragmentation into smaller sizes at the ice line. Collisions among larger parent bodies may also contribute to the small grain reservoir in the inner disk, but these parent bodies must be enstatite-poor. In addition, the variation between MIRI and Spitzer spectra can be explained by a combination of grain growth over 15 years and a dynamical inner disk where opacity changes occur resulting from the highly variable hot (T~1000 K) innermost dust reservoir.
Key words: methods: data analysis / methods: observational / protoplanetary disks / infrared: planetary systems
© The Authors 2024
Open Access article, published by EDP Sciences, under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
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