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arXiv 1303.3744astro-ph.SR
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原行星盘光谱中的69微米镁橄榄石带--Herschel DIGIT计划的结果

The 69 micron forsterite band in spectra of protoplanetary disks - Results from the Herschel DIGIT programme

B. Sturm, J. Bouwman, Th. Henning, N. J. Evans, L. B. F. M. Waters, E. F. van Dishoeck, J. D. Green, J. Olofsson, G. Meeus, K. Maaskant, C. Dominik, J. C. Auger… 展开作者

B. Sturm, J. Bouwman, Th. Henning, N. J. Evans, L. B. F. M. Waters, E. F. van Dishoeck, J. D. Green, J. Olofsson, G. Meeus, K. Maaskant, C. Dominik, J. C. Augereau, G. D. Mulders, B. Acke, B. Merin, G. J. Herczeg, The DIGIT team

摘要:

内容:我们分析了赫歇尔关键程序DIGIT中获得的32个围绕赫比格Ae/Be和T-Tauri星的拱星盘的赫歇尔PACS光谱。本文主要研究了硅酸镁橄榄石晶体的69 μ发射带。目的:这项工作提供了一个概述的69亩镁橄榄石带的DIGIT样品。我们的目标是推导出镁橄榄石颗粒的温度和成分。有了这些信息,就可以限制镁橄榄石在盘中的空间分布及其形成历史。研究方法:69 μ波段的位置和形状被用来通过与该波段的实验室光谱进行比较来推导尘埃的温度和成分。我们结合我们的数据与现有的斯皮策IRS光谱比较的存在和强度的69亩带的镁橄榄石波段在较短的波长。结果:共观察到32个发射源,其中8个发射带为69 μ,属于镁橄榄石。除了T-Tauri星AS 205之外,所有的探测都是针对与Herbig Ae/Be星相关的盘。产生69 μ条带的大多数镁橄榄石颗粒是温暖的(~100-200 K)和贫铁的(少于~2%铁)。只有AB-Aur需要大约3-4%的铁。结论:我们的研究结果支持了镁橄榄石颗粒在高温下通过平衡凝聚过程形成的假设。69和33 μ波段强度之间的联系表明,这些波段中至少有一部分发射来自相同的尘埃颗粒。此外,任何解释PACS和斯皮策IRS观测的模型都必须考虑波长依赖的光学深度的影响。我们发现69亩波段的检测率与宿主恒星的光谱类型的相关性的迹象。然而,我们的样本太小,无法获得明确的结果。

英文摘要:

Context: We have analysed Herschel-PACS spectra of 32 circumstellar disks around Herbig Ae/Be and T-Tauri stars obtained within the Herschel key programme DIGIT. In this paper we focus on the 69mu emission band of the crystalline silicate forsterite. Aims: This work provides an overview of the 69mu forsterite bands in the DIGIT sample. We aim to derive the temperature and composition of the forsterite grains. With this information, constraints can be placed on the spatial distribution of the forsterite in the disk and its formation history. Methods: Position and shape of the 69mu band are used to derive the temperature and composition of the dust by comparison to laboratory spectra of that band. We combine our data with existing Spitzer IRS spectra to compare the presence and strength of the 69mu band to the forsterite bands at shorter wavelengths. Results: A total of 32 sources have been observed, 8 of them show a 69mu emission band that can be attributed to forsterite. With the exception of the T-Tauri star AS205, all of the detections are for disks associated with Herbig Ae/Be stars. Most of the forsterite grains that give rise to the 69mu bands are warm (~100-200 K) and iron-poor (less than ~2% iron). Only AB-Aur requires approximately 3-4% of iron. Conclusions: Our findings support the hypothesis that the forsterite grains form through an equilibrium condensation process at high temperatures. The connection between the strength of the 69 and 33mu bands shows that at least part of the emission in these bands originates from the same dust grains. Further, any model that explains the PACS and the Spitzer IRS observations must take the effects of a wavelength dependent optical depth into account. We find indications of a correlation of the detection rate of the 69mu band with the spectral type of the host stars. However, our sample is too small to obtain a definitive result.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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