Evidence of a discontinuous disk structure around the Herbig Ae star HD 139614

The formation and evolution of a planetary system are intrinsically linked to the evolution of the primordial accretion disk and its dust and gas content. A new class of pre-main sequence objects has been recently identified as pre-transitional disks. They present near-infrared excess coupled to a f...

Full description

Saved in:
Bibliographic Details
Published inAstronomy and astrophysics (Berlin) Vol. 561; p. np
Main Authors Matter, A., Labadie, L., Kreplin, A., Lopez, B., Wolf, S., Weigelt, G., Ertel, S., Pott, J.-U., Danchi, W. C.
Format Journal Article
LanguageEnglish
Published Goddard Space Flight Center EDP Sciences 01.01.2014
Subjects
Online AccessGet full text

Cover

Loading…
More Information
Summary:The formation and evolution of a planetary system are intrinsically linked to the evolution of the primordial accretion disk and its dust and gas content. A new class of pre-main sequence objects has been recently identified as pre-transitional disks. They present near-infrared excess coupled to a flux deficit at about 10 microns and a rising mid-infrared and far-infrared spectrum. These features suggest a disk structure with inner and outer dust components, separated by a dust-depleted region (or gap). This could be the result of particular planet formation mechanisms that occur during the disk evolution. We here report on the first interferometric observations of the disk around the Herbig Ae star HD 139614. Its infrared spectrum suggests a flared disk, and presents pre-transitional features, namely a substantial near-infrared excess accompanied by a dip around 6 microns and a rising mid-infrared part. In this framework, we performed a study of the spectral energy distribution (SED) and the mid-infrared VLTI/MIDI interferometric data to constrain the spatial structure of the inner dust disk region and assess its possibly multi-component structure. We based our work on a temperature-gradient disk model that includes dust opacity. While we could not reproduce the SED and interferometric visibilities with a one-component disk, a better agreement was obtained with a two-component disk model composed of an optically thin inner disk extending from 0.22 to 2.3 AU, a gap, and an outer temperature-gradient disk starting at 5.6 AU. Therefore, our modeling favors an extended and optically thin inner dust component and in principle rules out the possibility that the near-infrared excess originates only from a spatially confined region. Moreover, the outer disk is characterized by a very steep temperature profile and a temperature higher than 300 K at its inner edge. This suggests the existence of a warm component corresponding to a scenario where the inner edge of the outer disk is directly illuminated by the central star. This is an expected consequence of the presence of a gap, thus indicative of a “pre-transitional” structure.
Bibliography:publisher-ID:aa22042-13
Present address: Institut de planétologie et d’astrophysique de Grenoble, 414 rue de la Piscine, Domaine universitaire, 38400 Saint-Martin-d’Hères, France.
dkey:10.1051/0004-6361/201322042
istex:840A9BE732C061637A6C9AF3E50BA87D31BB2AEF
ark:/67375/80W-JF1FTMRR-P
Based on observations collected at the European Southern Observatory, Chile (ESO IDs: 385.C-0886(A) and 087.C-0811(A)).
bibcode:2014A%26A...561A..26M
GSFC
Goddard Space Flight Center
GSFC-E-DAA-TN15090
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0004-6361
1432-0746
1432-0746
1432-0756
DOI:10.1051/0004-6361/201322042