论文标题

尘土环中的灰尘反馈触发的中尺度不稳定性:起源和观察性含义

Meso-scale Instability Triggered by Dust Feedback in Dusty Rings: Origin and Observational Implications

论文作者

Huang, Pinghui, Li, Hui, Isella, Andrea, Miranda, Ryan, Li, Shengtai, Ji, Jianghui

论文摘要

ALMA对原月球磁盘(PPD)的高空间分辨率观察已经揭示了许多细节,这些细节在磁盘物理学以及灰尘动态上提供了有趣的约束,这两个细节对于理解行星的形成至关重要。我们进行了高分辨率2D全球流体动力学模拟,包括尘埃反馈的影响,以研究尘土环的稳定性。当环边缘相对较锋利并且尘埃表面密度与气体表面密度相当时,我们发现尘埃反馈可以增强方位角速度曲线的径向梯度和环边缘处的潜在涡度曲线。这最终导致在中尺度上的不稳定性(几个磁盘尺度的空间尺度),导致尘土飞扬的环被许多紧凑型区域填充,其中许多紧凑型区域在中间尺度上具有高度浓缩的灰尘密度。我们还使用我们的模拟结果产生合成的灰尘发射图像,并讨论模拟和观察之间的比较。

High spatial resolution observations of protoplanetary disks (PPDs) by ALMA have revealed many details that are providing interesting constraints on the disk physics as well as dust dynamics, both of which are essential for understanding planet formation. We carry out high-resolution, 2D global hydrodynamic simulations, including the effects of dust feedback, to study the stability of dusty rings. When the ring edges are relatively sharp and the dust surface density becomes comparable to the gas surface density, we find that dust feedback enhances the radial gradients of both the azimuthal velocity profile and the potential vorticity profile at the ring edges. This eventually leads to instabilities on meso-scales (spatial scales of several disk scale heights), causing dusty rings to be populated with many compact regions with highly concentrated dust densities on meso-scales. We also produce synthetic dust emission images using our simulation results and discuss the comparison between simulations and observations.

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