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arXiv 0808.0619astro-ph
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探测IM Lupi星周盘中的尘埃颗粒演化。尘埃盘的多波长观测和模拟

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

C. Pinte, D. L. Padgett, F. Menard, K. R. Stapelfeldt, G. Schneider, J. Olofsson, O. Panic, J. C. Augereau, G. Duchene, J. Krist, K. Pontoppidan, M. D. Perrin, … 展开作者

C. Pinte, D. L. Padgett, F. Menard, K. R. Stapelfeldt, G. Schneider, J. Olofsson, O. Panic, J. C. Augereau, G. Duchene, J. Krist, K. Pontoppidan, M. D. Perrin, C. A. Grady, J. Kessler-Silacci, E. F. van Dishoeck, D. Lommen, M. Silverstone, D. C. Hines, S. Wolf, G. A. Blake, T. Henning, B. Stecklum

摘要:

我们提出了一个全色的研究,涉及多技术的方法,围绕金牛座T星IM狼(Sz 82)的拱盘。我们利用测光、分光、毫米干涉测量和多波长成像对Lupi IM进行了全面的观测研究。这是第一次,光盘是解决从光学和近红外波长的散射光,毫米制度的热发射。我们的数据集,结合现有的光度数据,提供了一个广泛的覆盖范围的光谱能量分布,包括硅酸盐发射带的详细光谱。我们进行了同步建模的各种观测,使用辐射转移代码MCFOST,并分析了网格模型的参数空间的很大一部分通过贝叶斯推断。我们已经建立了一个模型,可以重现所有的观察光盘。我们的分析说明了结合广泛的观察,以充分约束光盘模型的重要性,每个观察提供了一个强有力的约束,只有在某些方面的光盘结构和尘埃含量。尘埃演化在光盘的定量证据:晶粒生长到毫米级的颗粒,垂直分层的尘埃颗粒与微米颗粒接近光盘表面和较大的颗粒已经解决了对光盘中面,并可能形成蓬松的聚集体和/或周围的冰幔颗粒。

英文摘要:

We present a panchromatic study, involving a multiple technique approach, of the circumstellar disc surrounding the T Tauri star IM Lupi (Sz 82). 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. 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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