4.6 Article

Probing dust grain evolution in IM Lupi's circumstellar disc -: Multi-wavelength observations and modelling of the dust disc

期刊

ASTRONOMY & ASTROPHYSICS
卷 489, 期 2, 页码 633-650

出版社

EDP SCIENCES S A
DOI: 10.1051/0004-6361:200810121

关键词

circumstellar matter; accretion, accretion disks; planetary systems : protoplanetary disks; radiative transfer; stars : formation; pulsars : individual : IM Lupi

资金

  1. European Commission's Seventh Framework Program as a Marie Curie Intra-European Fellow [PIEF-GA-2008-220891]
  2. Agence Nationale pour la Recherche (ANR) of France [ANR-07-BLAN-0221]
  3. Association of Universities for Research in Astronomy, Inc.
  4. NASA contract [NAS 5-26555]
  5. STScI
  6. NASA [1224608, 1230779, 1256316]
  7. NSF
  8. Spitzer Postdoctoral Fellowship Program
  9. NWO Spinoza grant
  10. NOVA
  11. European Research Training Network
  12. PLANETS [HPRN-CT-2002-00308]
  13. [G0/7387]
  14. [GO/10177]

向作者/读者索取更多资源

Aims. We present a panchromatic study, involving a multiple technique approach, of the circumstellar disc surrounding the T Tauri star IM Lupi (Sz 82). Methods. We have undertaken a comprehensive observational study of IM Lupi using photometry, spectroscopy, millimetre interferometry and multi-wavelength imaging. For the first time, the disc is resolved from optical and near-infrared wavelengths in scattered light, to the millimetre regime in thermal emission. Our data-set, in conjunction with existing photometric data, provides an extensive coverage of the spectral energy distribution, including a detailed spectrum of the silicate emission bands. We have performed a simultaneous modelling of the various observations, using the radiative transfer code MCFOST, and analysed a grid of models over a large fraction of the parameter space via Bayesian inference. Results. We have constructed a model that can reproduce all of the observations of the disc. Our analysis illustrates the importance of combining a wide range of observations in order to fully constrain the disc model, with each observation providing a strong constraint only on some aspects of the disc structure and dust content. Quantitative evidence of dust evolution in the disc is obtained: grain growth up to millimetre-sized particles, vertical stratification of dust grains with micrometric grains close to the disc surface and larger grains which have settled towards the disc midplane, and possibly the formation of fluffy aggregates and/ or ice mantles around grains.

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