论文标题

TW Hya Rosetta Stone项目II:甲醛的空间分辨出在低温气相形成下的提示

The TW Hya Rosetta Stone Project II: Spatially resolved emission of formaldehyde hints at low-temperature gas-phase formation

论文作者

van Scheltinga, Jeroen Terwisscha, Hogerheijde, Michiel R., Cleeves, L. Ilsedore, Loomis, Ryan A., Walsh, Catherine, Öberg, Karin I., Bergin, Edwin A., Bergner, Jennifer B., Blake, Geoffrey A., Calahan, Jenny K., Cazzoletti, Paolo, van Dishoeck, Ewine F., Guzmán, Viviana V., Huang, Jane, Kama, Mihkel, Qi, Chunhua, Teague, Richard, Wilner, David J.

论文摘要

甲醛(h $ _2 $ co)是甲醇等有机物($ _3 $ oh)的重要先驱。重要的是要了解在恒星和行星形成期间产生H $ _2 $ CO和益生元分子的条件。 H $ _2 $ CO具有气相和固态地层途径,涉及UV生产的自由基前体或Co冰和冷($ \ Lessim 20 $ K)尘埃谷物。为了了解哪种途径占主导地位,气态H $ _2 $ CO的Ortho-Para比率(OPR)已用作探针,值为3表示“温暖”条件,$ <3 $链接到固体中的冷形成。我们介绍了在TW hya Protoplanetary磁盘中的多个Ortho-和para-h $ _2 $ CO转换的空间解决的ALMA观察结果,以测试行星形成期间的H $ _2 $ CO形成理论。我们发现磁盘平均旋转温度和列密度为$ 33 \ pm2 $ k,($ 1.1 \ pm0.1)\ times10^{12} $ cm $^{ - 2} $和$ 25 \ pm2 $ k,$(4.4 \ pm0.3) para-h $ _2 $ co,分别为$ 2.49 \ pm0.23 $的OPR。径向解析的分析表明,观察到的H $ _2 $ CO主要在30-40 K的旋转温度下排放,对应于$ z/r \ ge0.25 $的层。 OPR与60 au(卵石磁盘的程度)一致,并将超过60 au降低至$ 2.0 \ pm0.5 $。后者对应于12 K的自旋温度,远低于旋转温度。相对均匀的发射条件,OPR中的径向梯度以及升华后OPR比的最新实验实验和理论的结合,使我们推测,在TW YHYA磁盘上观察到的H $ _2 $ CO是造成观察到的H $ _2 $ CO的原因。

Formaldehyde (H$_2$CO) is an important precursor to organics like methanol (CH$_3$OH). It is important to understand the conditions that produce H$_2$CO and prebiotic molecules during star and planet formation. H$_2$CO possesses both gas-phase and solid-state formation pathways, involving either UV-produced radical precursors or CO ice and cold ($\lesssim 20$ K) dust grains. To understand which pathway dominates, gaseous H$_2$CO's ortho-to-para ratio (OPR) has been used as a probe, with a value of 3 indicating "warm" conditions and $<3$ linked to cold formation in the solid-state. We present spatially resolved ALMA observations of multiple ortho- and para-H$_2$CO transitions in the TW Hya protoplanetary disk to test H$_2$CO formation theories during planet formation. We find disk-averaged rotational temperatures and column densities of $33\pm2$ K, ($1.1\pm0.1)\times10^{12}$ cm$^{-2}$ and $25\pm2$ K, $(4.4\pm0.3)\times10^{11}$ cm$^{-2}$ for ortho- and para-H$_2$CO, respectively, and an OPR of $2.49\pm0.23$. A radially resolved analysis shows that the observed H$_2$CO emits mostly at rotational temperatures of 30-40 K, corresponding to a layer with $z/R\ge0.25$. The OPR is consistent with 3 within 60 au, the extent of the pebble disk, and decreases beyond 60 au to $2.0\pm0.5$. The latter corresponds to a spin temperature of 12 K, well below the rotational temperature. The combination of relatively uniform emitting conditions, a radial gradient in the OPR, and recent laboratory experiments and theory on OPR ratios after sublimation, lead us to speculate that gas-phase formation is responsible for the observed H$_2$CO across the TW Hya disk.

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