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arXiv 1301.6876astro-ph.SRastro-ph.EP
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HD 113766 A周围的双重碎片盘-VLTI/Midi和Herschel/Pacs观察到的热和冷尘埃

The twofold debris disk around HD 113766 A - Warm and cold dust as seen with VLTI/Midi and Herschel/Pacs

Johan Olofsson, Thomas Henning, Markus Nielbock, Jean-Charles Augereau, Attila Juhasz, Isa Oliveira, Olivier Absil, Akemi Tamanai

摘要:

温暖的碎片磁盘是一个子样本的大量人口的碎片磁盘,并显示多余的发射中红外线。在太阳型恒星周围,很少有物体显示发射功能中红外光谱观测,这是由于小,温暖的硅酸盐尘埃颗粒。这种温暖尘埃的起源可能是由几个物体之间的碰撞或由外部带的运输来解释的。我们提出并分析了新的远红外赫歇尔/Pacs观测结果,并补充了中红外(VLTI/Midi和VLT/Visir)的地基数据,这些罕见的系统之一:HD 113766 A周围的10- 1600万年前的碎片盘。我们改进了现有的模型来解释这些新的观测结果,并更好地约束尘埃及其成分的空间分布。我们强调SED建模的局限性和空间分辨观测的必要性。我们发现,该系统最好由位于第一个AU内的内盘和位于9-13 AU之间的外盘来描述,内盘受到Midi数据的良好约束。在内部尘埃带,我们以前发现的富铁结晶橄榄石颗粒仍然成立。我们没有观察到的时间变化的排放功能超过至少8年的时间跨度,在一个环境中受到强辐射压力。发射特征的时间稳定性表明,微米级的尘埃颗粒不断从同一个水库补充,亚微米级的颗粒可能耗尽。我们认为,发射功能可能来自多组分聚集体。我们讨论可能的情况下,温暖的尘埃的起源。Midi探测到的最内部区域的致密性以及尘埃成分表明,我们正在目睹部分分化的天体之间(至少)一次碰撞的结果,在一个可能因地球行星形成而变得不稳定的环境中。

英文摘要:

Warm debris disks are a sub-sample of the large population of debris disks, and display excess emission in the mid-IR. Around solar-type stars, very few objects show emission features in mid-IR spectroscopic observations, that are attributed to small, warm silicate dust grains. The origin of this warm dust can possibly be explained either by a collision between several bodies or by transport from an outer belt. We present and analyse new far-IR Herschel/Pacs observations, supplemented by ground-based data in the mid-IR (VLTI/Midi and VLT/Visir), for one of these rare systems: the 10-16 Myr old debris disk around HD 113766 A. We improve an existing model to account for these new observations, and better constrain the spatial distribution of the dust and its composition. We underline the limitations of SED modelling and the need for spatially resolved observations. We find that the system is best described by an inner disk located within the first AU, well constrained by the Midi data, and an outer disk located between 9-13 AU. In the inner dust belt, our previous finding of Fe-rich crystalline olivine grains still holds. We do not observe time variability of the emission features over at least a 8 years time span, in a environment subjected to strong radiation pressure. The time stability of the emission features indicates that μm-sized dust grains are constantly replenished from the same reservoir, with a possible depletion of sub-μm-sized grains. We suggest that the emission features may arise from multi-composition aggregates. We discuss possible scenarios concerning the origin of the warm dust. The compactness of the innermost regions as probed by Midi, as well as the dust composition, suggest that we are witnessing the outcomes of (at least) one collision between partially differentiated bodies, in an environment possibly rendered unstable by terrestrial planetary formation.

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