动态HD 100453盘上的冰升华揭示了遗传复杂有机物的丰富储存库

Alice S. Booth, Lisa Wölfer, Milou Temmink, Jenny Calahan, Lucy Evans, Charles J. Law, Margot Leemker, Shota Notsu, Karin Öberg and Catherine Walsh
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摘要

明亮的年轻a型恒星周围的原行星盘是确定行星形成过程中存在的复杂有机分子(COMs)丰度的主要观测实验室。与低质量恒星相比,这些较热的圆盘包含复杂分子的升华前沿,如CH3OH,在空间尺度上可以通过阿塔卡马大型毫米/亚毫米阵列(ALMA)获得。我们展示了对赫比格Ae盘HD 100453的ALMA观测,揭示了从尘埃腔边缘升华的丰富的COMs储存库。除CH3OH外,我们首次在II类圆盘中检测到13CH3OH,揭示了圆盘大型有机物中13C的3倍增强因子。对CH2DOH的初步探测也有报道,结果的D/H为1%-2%,这与分子云中低温CH3OH形成所预期的氘增强以及在彗星中测量到的CH3OH氘化一致。甲酸甲酯(CH3OCHO)的检测,只有几个百分点的CH3OH水平,比其他富含有机物的赫比格Ae盘低一个数量级,但更符合恒星形成早期阶段的有机丰度模式。这些数据一起提供了多种证据,证明圆盘,也就是行星和彗星形成的材料,包含了继承的星际冰,这可能是迄今为止最有力的证据,表明大部分星际有机冰成分在行星形成的早期阶段幸存下来。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Ice Sublimation in the Dynamic HD 100453 Disk Reveals a Rich Reservoir of Inherited Complex Organics
Protoplanetary disks around luminous young A-type stars are prime observational laboratories to determine the abundances of complex organic molecules (COMs) present during planet formation. In contrast to their lower stellar mass counterparts, these warmer disks contain the sublimation fronts of complex molecules such as CH3OH on spatial scales accessible with the Atacama Large Millimeter/submillimeter Array (ALMA). We present ALMA observations of the Herbig Ae disk HD 100453 that uncover a rich reservoir of COMs sublimating from the dust cavity edge. In addition to CH3OH, we detect 13CH3OH for the first time in a Class II disk, revealing a factor of three enhancement of 13C in the disk large organics. A tentative detection of CH2DOH is also reported, resulting in a D/H of 1%–2%, which is consistent with the expected deuterium enhancement from the low-temperature CH3OH formation in molecular clouds and with the deuteration of CH3OH measured in comets. The detection of methyl-formate (CH3OCHO), at only a few percent level of CH3OH, is an order of magnitude lower compared to claims toward other organic-rich Herbig Ae disks but is more in line with organic abundance patterns toward the earlier stages of star formation. Together these data provide multiple lines of evidence that disks, and therefore the planet- and comet-forming materials, contain inherited interstellar ices and perhaps the strongest evidence to date that much of the interstellar organic ice composition survives the early stages of planet formation.
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