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arXiv 2106.12947astro-ph.EPastro-ph.SR
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HD 179218的第一个MATISSE L波段观测。内10金区是否富含碳尘埃粒子?

First MATISSE L-band observations of HD 179218. Is the inner 10 au region rich in carbon dust particles?

E. Kokoulina, A. Matter, B. Lopez, E. Pantin, N. Ysard, G. Weigelt, E. Habart, J. Varga, A. Jones, A. Meilland, E. Dartois, L. Klarmann, J. -C. Augereau, R. van… 展开作者

E. Kokoulina, A. Matter, B. Lopez, E. Pantin, N. Ysard, G. Weigelt, E. Habart, J. Varga, A. Jones, A. Meilland, E. Dartois, L. Klarmann, J. -C. Augereau, R. van Boekel, M. Hogerheijde, G. Yoffe, L. B. F. M. Waters, C. Dominik, W. Jaffe, F. Millour, Th. Henning, K. -H. Hofmann, D. Schertl, S. Lagarde, R. G. Petrov, P. Antonelli, F. Allouche, P. Berio, S. Robbe-Dubois, P. Abraham, U. Beckmann, A. Bensberg, F. Bettonvil, P. Bristow, P. Cruzalèbes, W. C. Danchi, M. Dannhoff, U. Graser, M. Heininger, L. Labadie, M. Lehmitz, C. Leinert, K. Meisenheimer, C. Paladini, I. Percheron, Ph. Stee, J. Woillez, S. Wolf, G. Zins, M. Delbo, J. Drevon, J. Duprat, V. Gámez Rosas, V. Hocdé, J. Hron, C. A. Hummel, J. W. Isbell, J. Leftley, A. Soulain, F. Vakili, M. Wittkowski

摘要:

碳是宇宙中最丰富的成分之一。虽然硅酸盐一直是原行星盘(PPD)中固相研究的主要焦点,但对固体碳含量,特别是在行星形成区域($\sim $ 0.1至10 au)的固体碳含量知之甚少。幸运的是,几种难熔碳质物质存在C-H键(例如氢化纳米金刚石和无定形碳以及多环芳烃(PAH)),其产生的红外(IR)特征可用于追踪固体碳储层。新的中红外仪器MATISSE,安装在甚大望远镜干涉仪(VLTI),可以在空间上解决内部区域($\sim$ 1至10 au)的PPD和定位,下降到au尺度,来自碳颗粒的排放。我们的目的是提供一个一致的看法,径向结构,下降到au尺度,以及基本的物理性质和性质的材料负责的红外连续辐射在内部磁盘区域周围HD 179218。我们实现了一个温度梯度模型来解释磁盘红外连续发射,基于多波长数据集,包括宽带光谱能量分布(SED)和VLTI的H-,L-和N-波段的干涉数据在低光谱分辨率。然后,我们添加了一个环状组件,代表碳质L-波段特征发射区域,以评估其可探测性,在未来更高的光谱分辨率观测采用中红外干涉。

英文摘要:

Carbon is one of the most abundant components in the Universe. While silicates have been the main focus of solid phase studies in protoplanetary discs (PPDs), little is known about the solid carbon content especially in the planet-forming regions ($\sim $0.1 to 10 au). Fortunately, several refractory carbonaceous species present C-H bonds (such as hydrogenated nano-diamond and amorphous carbon as well as polycyclic aromatic hydrocarbons (PAHs)), which generate infrared (IR) features that can be used to trace the solid carbon reservoirs. The new mid-IR instrument MATISSE, installed at the Very Large Telescope Interferometer (VLTI), can spatially resolve the inner regions ($\sim$ 1 to 10 au) of PPDs and locate, down to the au-scale, the emission coming from carbon grains. Our aim is to provide a consistent view on the radial structure, down to the au-scale, as well as basic physical properties and the nature of the material responsible for the IR continuum emission in the inner disk region around HD 179218. We implemented a temperature-gradient model to interpret the disk IR continuum emission, based on a multiwavelength dataset comprising a broadband spectral energy distribution (SED) and VLTI H-, L-, and N-bands interferometric data obtained in low spectral resolution. Then, we added a ring-like component, representing the carbonaceous L-band features-emitting region, to assess its detectability in future higher spectral resolution observations employing mid-IR interferometry.

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