论文标题

在热核中解析复杂有机分子的解吸:从非热解到热解吸或两步热解吸的过渡?

Resolving desorption of complex organic molecules in a hot core: Transition from non-thermal to thermal desorption or two-step thermal desorption?

论文作者

Busch, Laura A., Belloche, Arnaud, Garrod, Robin T., Müller, Holger S. P., Menten, Karl M.

论文摘要

使用ALMA干涉仪提供的高角度分辨率,我们希望在热分子核心Sagittarius B2(N1)中解析COM发射,从而阐明了在热核中复杂有机分子(COM)的解吸过程。我们将数据作为3 mM光谱线调查的一部分,与ALMA(REMOCA)重新探索分子复杂性,以研究Sagittarius B2(N1)中COM发射的形态。在LTE的假设下对十个COM的光谱进行了建模,并从连续峰的南部和西部的各个距离都得出了种群图。基于此分析,得出了分析的COM旋转温度和COM丰度曲线。基于形态,可以进行粗略的分离,以分为O-和N含N的COM。温度曲线与光学厚度灰尘的信封的原始加热的期望一致。丰富的概况反映了与形态中所见的类似趋势,并且在很大程度上与天体化学模型的结果一致,这些模型除了与水的共同点外,还可以预测,O-bareation Coms主要在低温下在低温下的防尘粒表面上形成,而至少在某些N-N-BEARIN COM和CH $ _3 $ CHO的高度阶段形成了更高的气相。与模型预测相比,我们的观察结果表明,在灰尘晶粒在距离差异约100 k的谷物表面上,可能与水一起在灰尘晶粒上形成的COM可能与水旁边。低于〜100 k的非零丰度值表明在这些低温下正在起作用的另一个解吸过程:非热解吸或与COM在外部水位贫困冰层中经历的较低结合能有关的部分热解吸。无论哪种情况,这都是第一次在com解吸方面之间的过渡已在热核中解决。

Using the high angular resolution provided by the ALMA interferometre we want to resolve the COM emission in the hot molecular core Sagittarius B2(N1) and thereby shed light on the desorption process of Complex Organic Molecules (COMs) in hot cores. We use data taken as part of the 3 mm spectral line survey Re-exploring Molecular Complexity with ALMA (ReMoCA) to investigate the morphology of COM emission in Sagittarius B2(N1). Spectra of ten COMs are modelled under the assumption of LTE and population diagrams are derived for positions at various distances to the south and west from the continuum peak. Based on this analysis, resolved COM rotation temperature and COM abundance profiles are derived. Based on the morphology, a rough separation into O- and N-bearing COMs can be done. Temperature profiles are in agreement with expectations of protostellar heating of an envelope with optically thick dust. Abundance profiles reflect a similar trend as seen in the morphology and, to a great extent, agree with results of astrochemical models that, besides the co-desorption with water, predict that O-bearing COMs are mainly formed on dust grain surfaces at low temperatures while at least some N-bearing COMs and CH$_3$CHO are substantially formed in the gas phase at higher temperatures. Our observational results, in comparison with model predictions, suggest that COMs that are exclusively or to a great extent formed on dust grains desorb thermally at ~100 K from the grain surface likely alongside water. Non-zero abundance values below ~100 K suggest that another desorption process is at work at these low temperatures: either non-thermal desorption or partial thermal desorption related to lower binding energies experienced by COMs in the outer, water-poor ice layers. In either case, this is the first time that the transition between two regimes of COM desorption has been resolved in a hot core.

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