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arXiv 2409.04575astro-ph.SRastro-ph.GA
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极低光度天体中的爆发后化学:一氧化氮的异常高丰度

Post-Outburst Chemistry in a Very Low-Luminosity Object: Peculiar High Abundance of Nitric Oxide

B. M. Kulterer, S. F. Wampfler, N. F. W. Ligterink, N. Murillo, T. -H. Hsieh, M. K. McClure, A. Boogert, K. Kipfer, P. Bjerkeli, M. N. Drozdovskaya

AI总结:

本研究利用APEX观测极低光度天体DC3272+18的爆发后化学,首次探测到一氧化氮(NO),发现其可能源于冰升华后的光解产物,并指出NO有望作为追踪爆发源水雪线的探针。

摘要:

摘要:极低光度天体(VeLLOs)是深嵌且极暗的天体,被认为处于间歇性吸积过程的静息阶段。它们填补了我们对恒星形成理解上的一个重要空白。孤立DC3272+18云中的VeLLO经历过一次爆发,因此是研究此类天体气相化学组成的理想目标。我们利用Atacama Pathfinder EXperiment (APEX)在213.6--272.4 GHz频率范围内的四个光谱窗口进行了观测,旨在识别可直接与过去爆发相关的分子,利用探测到的谱线通量、柱密度和丰度比来表征VeLLO的不同物理成分,并探测复杂有机分子的存在。首次在此类源中探测到一氧化氮(NO),其形成可能是由爆发期间颗粒表面物质的升华引起的。气相中直接形成NO的途径,来自冰中H2O和NH3升华后产生的光解产物。尽管当前的水雪线可能已退缩至爆发前的小半径,但挥发性NO物质仍广泛存在于气相中,观测中其相对于甲醇的高柱密度证明了这一点。这表明NO可能被用来追踪爆发源中的水雪线。为了排除也可能导致NO形成的非热脱附过程,必须通过未来更高空间分辨率的观测以及在更多目标中寻找NO来验证这一提议。

英文摘要:

Abridged: Very Low Luminosity Objects (VeLLOs) are deeply embedded, and extremely faint objects and are thought to be in the quiescent phase of the episodic accretion process. They fill an important gap in our understanding of star formation. The VeLLO in the isolated DC3272+18 cloud has undergone an outburst, and is thus an ideal target for investigating the chemical inventory in the gas phase of an object of its type. Observations with the Atacama Pathfinder EXperiment (APEX) in four spectral windows in the frequency range of 213.6--272.4~GHz have been carried out to identify molecules that can be directly linked to the past outburst, utilize the line fluxes, column densities, and the abundance ratios of the detected species to characterize the different physical components of the VeLLO, and probe for the presence of complex organic molecules. Nitric oxide (NO) is detected for the first time in a source of this type, and its formation could be induced by the sublimation of grain-surface species during the outburst. A pathway to form NO directly in the gas phase is from the photodissociation products created after the sublimation of H$_2$O and NH$_3$ from the ices. While the present time water snowline has likely retreated to pre-outburst small radius, the volatile NO species is still extensively present in the gas phase, as evident by its high column density relative to methanol in the observations. This suggests that NO could be potentially used to trace the water snowline in outbursting sources. In order to rule out non-thermal desorption processes that could also have led to the formation of NO, this proposition has to be verified with future observations at higher spatial resolution, and by searching for NO in additional targets.

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