论文标题
用阿尔玛和下一代探测原行星磁盘中死区的内边缘
Probing Inner-Edge of Dead Zones in Protoplanetary Disks with ALMA and Next Generation Very Large Array
论文作者
论文摘要
使用阿尔玛(Alma)的原月球磁盘发现子结构为我们提供了对行星形成的关键见解。但是,关于岩石行星形成的观察性约束仍然很少,尤其是因为空间分辨率有限。所谓的死区的内边缘是岩石行星形成的优先地点之一。我们研究了Alma和NGVLA的能力,可以观察到Herbig Star周围死区的内边缘预期的灰尘浓度。 Herbig ae/be恒星是探索岩石谷物在原球门磁盘中的演变的有用实验室,因为它们的高光度高光度,从而将死区的内边缘向外推动。我们发现,由于其前所未有的角度分辨率和灵敏度,NGVLA可以检测到死区内边缘处的灰尘浓度,其合理的整合时间为$λ= 3,7 $ mm和1 cm。预计尘埃浓度将在ALMA波长处光亮厚,并且由于其分辨率有限,因此无法在空间上解决。另一方面,内部磁盘区域的通量密度($ \ sim $ 3--4 au)对带有灰尘环的磁盘观察到的磁盘较高,因此将是一个有用的指标,可以帮助我们选择潜在的磁盘候选磁盘,在内部最多区域具有灰尘浓度。通过这些观察,我们可以表征最内向的磁盘区域中尘埃浓度的过程,岩石行星可以形成。
The discovery of substructures in protoplanetary disks with ALMA has provided us key insights on the formation of planets. However, observational constraints on the formation of rocky planets have been still sparse, especially because of the limited spatial resolution. The inner edge of so-called dead zone is one of the preferential sites of rocky planet formation. We investigate the capabilities of ALMA and ngVLA for observing a dust concentration expected at the inner edge of the dead-zone around a Herbig star. Herbig Ae/Be stars are useful laboratories for exploring the evolution of rocky grains in protoplanetary disks because of their high luminosity which pushes the dead-zone inner edge outward. We find that, thanks to its unprecedented angular resolution and sensitivity, ngVLA can detect the dust concentration at the dead-zone inner edge, with a reasonable integration time of 10 hrs at $λ=3,7$ mm and 1 cm. The dust concentration is expected to be optically thick at the ALMA wavelengths and cannot be spatially resolved due to its limited resolution. On the other hand, the flux density from the inner disk regions ($\sim$3--4 au) observed with current VLA is higher for disks with a dust ring, and hence would be a useful indicator that help us choose potential candidates of disks having a dust concentration at the inner most region. With these observations we can characterize the process of dust concentration in the innermost disk regions, where rocky planets can form.