论文标题

原星磁盘内部区域的演变

The Evolution Of The Inner Regions of Protoplanetary Disks

论文作者

Manzo-Martínez, Ezequiel, Calvet, Nuria, Hernández, Jesús, Lizano, Susana, Hernández, Ramiro Franco, Miller, Christopher J., Maucó, Karina, Briceño, César, D'Alessio, Paola

论文摘要

我们介绍了一项研究,对低质量恒星周围的原星盘的内部几个天文单位的演变。我们考虑附近的恒星群体,年龄从1到11个MYR,分布成四个年龄箱。将Panstars光度法与光谱类型相结合,我们为每个恒星始终如一地得出红色的变红,我们使用(1)用它来测量Photosphere上方的过量发射,并通过新的IR过量指标和(2)估算H $α$α$α$α$α$α$α$α$α$α$α$α$α$α$α$α$α$α$α$α$α$α$α$α$α$的质量增生率($ \ dot {m} $)。使用观察到的$ \ dot {m} $的衰减作为固定粘性进化模型的初始条件和粘度参数的约束,我们使用近似贝叶斯建模来推断产生观察到的IR随着年龄降低的灰尘特性,在4.5至$ 24 \,μm中,范围为4.5至$ 24。我们计算具有两层壁的辐照盘模型的广泛网格,以模拟弯曲的灰尘内边缘,并获得与粘性进化预测的表面密度一致的垂直结构。我们发现,磁盘上层中的灰尘耗竭为$ε\ sim 3 \ times 10^{ - 3} $在1.5 Myr,与以前的研究一致,并且降至$ε\ sim 3 \ sim 3 \ times 10^{ - 4} $ 7.5 Myr。我们将光蒸发包括在磁盘演化的简单模型中,并发现光蒸发量质量损失速率为$ \ sim 1 -3 \ times 10 ^{ - 9} \,m _ {\ odot} yr ^{ - 1} $符合磁盘分数符合年龄的降低。这些模型显示了H $ _2 $ O和CO雪线的内向演变。

We present a study of the evolution of the inner few astronomical units of protoplanetary disks around low-mass stars. We consider nearby stellar groups with ages spanning from 1 to 11 Myr, distributed into four age bins. Combining PANSTARSS photometry with spectral types, we derive the reddening consistently for each star, which we use (1) to measure the excess emission above the photosphere with a new indicator of IR excess and (2) to estimate the mass accretion rate ($\dot{M}$) from the equivalent width of the H$α$ line. Using the observed decay of $\dot{M}$ as a constrain to fix the initial conditions and the viscosity parameter of viscous evolutionary models, we use approximate Bayesian modeling to infer the dust properties that produce the observed decrease of the IR excess with age, in the range between 4.5 and $24\,μ$m. We calculate an extensive grid of irradiated disk models with a two-layered wall to emulate a curved dust inner edge and obtain the vertical structure consistent with the surface density predicted by viscous evolution. We find that the median dust depletion in the disk upper layers is $ε\sim 3 \times 10^{-3}$ at 1.5 Myr, consistent with previous studies, and it decreases to $ε\sim 3 \times 10^{-4}$ by 7.5 Myr. We include photoevaporation in a simple model of the disk evolution and find that a photoevaporative wind mass-loss rate of $\sim 1 -3 \times 10 ^{-9} \, M_{\odot}yr^{-1}$ agrees with the decrease of the disk fraction with age reasonably well. The models show the inward evolution of the H$_2$O and CO snowlines.

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