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首页> 外文期刊>The Astrophysical journal >Gas Density Perturbations Induced by One or More Forming Planets in the AS 209 Protoplanetary Disk as Seen with ALMA
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Gas Density Perturbations Induced by One or More Forming Planets in the AS 209 Protoplanetary Disk as Seen with ALMA

机译:用ALMA观测到,AS 209初行星盘中一个或多个形成行星引起的气体密度扰动

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The formation of planets occurs within protoplanetary disks surrounding young stars, resulting in perturbation of the gas and dust surface densities. Here we report the first evidence of spatially resolved gas surface density (Σ g ) perturbation toward the AS?209 protoplanetary disk from the optically thin C18O (J?=?2?1) emission. The observations were carried out at 1.3 mm with Atacama Large Millimeter/submillimeter Array at a spatial resolution of about 03?×?02 (corresponding to ~38?×?25 au). The C18O emission shows a compact (≤60 au), centrally peaked emission and an outer ring peaking at 140 au, consistent with that observed in the continuum emission, and its azimuthally averaged radial intensity profile presents a deficit that is spatially coincident with the previously reported dust map. This deficit can only be reproduced with our physico-thermochemical disk model by lowering Σgas by nearly an order of magnitude in the dust gaps. Another salient result is that, contrary to C18O, the DCO+ (J?=?3?2) emission peaks between the two dust gaps. We infer that the best scenario to explain our observations (C18O deficit and DCO+ enhancement) is a gas perturbation due to one or more forming planets, which is commensurate with previous continuum observations of the source along with hydrodynamical simulations. Our findings confirm that the previously observed dust gaps are very likely due to perturbation of the gas surface density that is induced by a planet of at least 0.2M J in formation. Finally, our observations also show the potential of using CO isotopologues to probe the presence of one or more Saturn-mass planets.
机译:行星的形成发生在围绕年轻恒星的原行星盘内,导致气体和尘埃表面密度的扰动。在这里,我们报告了从光学上稀薄的C18O(Jα=?2?1)发射向AS?209原行星盘的空间分辨气体表面密度(Σg)扰动的第一个证据。用Atacama大毫米/亚毫米阵列在1.3mm处进行观察,其空间分辨率约为03××02(相当于〜38××25 au)。 C18O发射显示致密(≤60au),中心出现发射峰,外环在140 au出现峰,与连续发射中观察到的一致,并且其方位平均径向强度分布呈现与先前空间上重合的赤字报告尘埃图。这种缺陷只能通过我们的物理-热化学圆盘模型通过将∑gas降低尘埃间隙近一个数量级来再现。另一个明显的结果是,与C18O相反,两个尘埃间隙之间的DCO +(Jα=?3?2)发射峰。我们推断,解释我们的观测值(C18O缺乏和DCO +增强)的最佳方案是由于一个或多个行星形成而引起的气体扰动,这与先前对源的连续观测和流体动力学模拟相称。我们的发现证实,先前观察到的尘埃间隙很可能是由于形成至少0.2M J的行星引起的气体表面密度扰动。最后,我们的观察结果还显示了使用CO同位素同位素探测一个或多个土星质量行星的存在的潜力。

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