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Constraints from Dust Mass and Mass Accretion Rate Measurements on Angular Momentum Transport in Protoplanetary Disks

机译:尘埃质量和质积率测量对原行星盘角动量传输的约束

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摘要

In this paper, we investigate the relation between disk mass and mass accretion rate to constrain the mechanism of angular momentum transport in protoplanetary disks. We find a correlation between dust disk mass and mass accretion rate in Chamaeleon I with a slope that is close to linear, similar to the one recently identified in Lupus. We investigate the effect of stellar mass and find that the intrinsic scatter around the best-fit M-dust-M star and M-acc-M star relations is uncorrelated. We simulate synthetic observations of an ensemble of evolving disks using a Monte Carlo approach and find that disks with a constant alpha viscosity can fit the observed relations between dust mass, mass accretion rate, and stellar mass but overpredict the strength of the correlation between disk mass and mass accretion rate when using standard initial conditions. We find two possible solutions. In the first one, the observed scatter in M-dust and M-acc is not primordial, but arises from additional physical processes or uncertainties in estimating the disk gas mass. Most likely grain growth and radial drift affect the observable dust mass, while variability on large timescales affects the mass accretion rates. In the second scenario, the observed scatter is primordial, but disks have not evolved substantially at the age of Lupus and Chamaeleon I owing to a low viscosity or a large initial disk radius. More accurate estimates of the disk mass and gas disk sizes in a large sample of protoplanetary disks, through either direct observations of the gas or spatially resolved multiwavelength observations of the dust with ALMA, are needed to discriminate between both scenarios or to constrain alternative angular momentum transport mechanisms such as MHD disk winds.
机译:在本文中,我们研究了圆盘质量与质量增加率之间的关系,以限制原行星圆盘中角动量传输的机理。我们发现Chamaeleon I尘埃盘质量与吸积率之间的相关性接近线性,类似于最近在狼疮中发现的那样。我们研究了恒星质量的影响,发现围绕最合适的M-dust-M星和M-acc-M星关系的固有散射是不相关的。我们使用蒙特卡洛方法模拟了一组不断演化的磁盘的综合观测结果,发现具有恒定α粘度的磁盘可以满足所观察到的尘埃质量,吸积率和恒星质量之间的关系,但过高地预测了磁盘质量之间的相关强度使用标准初始条件时的质量增加率。我们找到两种可能的解决方案。在第一个中,观察到的M-灰尘和M-acc的散布不是原始的,而是由于附加的物理过程或估算磁盘气体质量的不确定性而产生的。晶粒长大和径向漂移最有可能影响可观察到的粉尘质量,而较大时间尺度上的变化会影响质量增加率。在第二种情况下,观察到的散射是原始的,但是由于粘度低或初始圆盘半径大,在红斑狼疮和Chamaeleon I时代,圆盘基本上没有演化。需要通过直接观测气体或使用ALMA对粉尘进行空间分辨的多波长观测来对大量原行星盘样品中的盘质量和气盘尺寸进行更准确的估算,以区分这两种情况或限制替代的角动量MHD磁盘风等传输机制。

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