Volume 334, Issue 9 pp. 912-915
Original Paper

Probing the temporal and spatial variations of dust emission in the protoplanetary disk of DG Tau with VLTI/MIDI: Preliminary results

K. É. Gabányi

Corresponding Author

K. É. Gabányi

MTA Research Centre for Astronomy and Earth Sciences, Konkoly Thege Miklós Astronomical Institute, H-1121 Konkoly Thege Miklós út 15-17, Budapest, Hungary

MTA Research Centre for Astronomy and Earth Sciences, Konkoly Thege Miklós Astronomical Institute, H-1121 Konkoly Thege Miklós üt 15-17, Budapest, HungarySearch for more papers by this author
L. Mosoni

L. Mosoni

MTA Research Centre for Astronomy and Earth Sciences, Konkoly Thege Miklós Astronomical Institute, H-1121 Konkoly Thege Miklós út 15-17, Budapest, Hungary

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A. Juhász

A. Juhász

Leiden Observatory, Leiden University, PO Box 9513, 2300 RA Leiden, The Netherlands

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P. Ábrahám

P. Ábrahám

MTA Research Centre for Astronomy and Earth Sciences, Konkoly Thege Miklós Astronomical Institute, H-1121 Konkoly Thege Miklós út 15-17, Budapest, Hungary

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Th. Ratzka

Th. Ratzka

Universitäts-Sternwarte München, Ludwig-Maximilians-Universität München, Scheinerstr 1, D-81679 München, Germany

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N. Sipos

N. Sipos

Institute for Astronomy, ETH Zürich, Wolfgang-Pauli-Straße 27, CH-8093 Zürich, Switzerland

Universität Göttingen, Institut für Astrophysik, Friedrich-Hund-Platz 1, D-37077 Göttingen, Germany

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R. van Boekel

R. van Boekel

Max-Planck-Institut für Astronomie, D-69117 Heidelberg, Königstuhl 17, Germany

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W. Jaffe

W. Jaffe

Institute for Astronomy, ETH Zürich, Wolfgang-Pauli-Straße 27, CH-8093 Zürich, Switzerland

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First published: 07 November 2013

Abstract

The signatures of dust processing and grain growth – related to the formation of rocky planets – are easily seen in midinfrared spectral features. One important diagnostic tool in this context is the silicate feature in the spectra of young stellar objects (YSO). The low-mass YSO, DG Tau shows unique temporal variations in its silicate feature. We conducted multi-epoch observations of DG Tau with the MID-Infrared Interferometric instrument of the Very Large Telescope Interferometer to obtain the spectra of the inner and outer disk regions in order to investigate where the previously reported variations of the silicate feature originate from. Here we present the preliminary results of the first two epochs of observations. We found that on a time-scale of two months, the source showed significant brightening. At the same time the mid-infrared emitting region expanded. While the identification of the silicate feature is difficult, our results qualitatively agree with the scenario explaining the varying silicate feature with dust lifted up above the disk. (© 2013 WILEY-VCH Verlag GmbH & Co. KGaA, Weinheim)

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