arXivDaily arXiv每日学术速递 周一至周五更新
arXiv 1302.1389astro-ph.SR
收藏

年轻原恒星周围过渡盘中的氢释放行星

Hydrogen-loosing planets in transition discs around young protostars

Sergei Nayakshin

摘要:

我们指出,在潮汐缩小(TD)理论框架内产生的行星形成的原行星发挥了非常重要的作用,吸积盘的演变托管他们。由于所有TD原行星最初的质量都与$\sim 10$木星的质量一样,它们能够在圆盘上打开非常深的缝隙,甚至完全隔离内部圆盘的流动。此外,与其他行星形成理论不同,TD原行星是其原恒星的质量捐赠者。行星被原恒星吞噬的一个潜在的可观察到的特征是FU Ori样的爆发,以及更普遍的原恒星吸积,正如一些作者最近所讨论的那样。在这里,我们探讨TD假说的另一个观测意义:尘埃贫内吸积流,我们相信这可能是相关的一些观察到的毫米明亮的过渡盘周围的原恒星。在我们的模型中,一颗巨大的原行星打断了其原恒星上富含尘埃的外盘的流动,同时将其贫尘埃包层的一部分释放到内盘中。然后,这就为观察到的气体而非尘埃吸积到恒星上提供了动力。经过更详细的研究,我们发现这种情况对于年轻的大质量盘是很自然的,但对于较老的盘就不那么自然了,那些自我吸引阶段在一百万年前或更久以前就结束了的人。这源于这样一个事实,即这样一个年龄的TD原行星应该已经显著收缩,因此不太可能失去太多的质量。因此,我们的结论是,要么(i)人口的“过渡盘”与大孔和灰尘贫吸积比通常认为的要年轻得多;或(ii)有一个知之甚少的阶段,后期删除灰尘贫信封TD行星;(iii)另一种解释的意见是正确的。

英文摘要:

We point out that protoplanets created in the framework of the Tidal Downsizing (TD) theory for planet formation play a very important role for the evolution of accretion discs hosting them. Since all TD protoplanets are initially as massive as $\sim 10$ Jupiter masses, they are able to open very deep gaps in their discs, and even completely isolate the inner disc flows from the outer ones. Furthermore, in contrast to other planet formation theories, TD protoplanets are mass donors for their protostars. One potentially observable signature of planets being devoured by their protostars are FU Ori like outbursts, and episodic protostar accretion more generally, as discussed by a number of authors recently. Here we explore another observational implication of TD hypothesis: dust poor inner accretion flows, which we believe may be relevant to some of the observed mm-bright transitional discs around protostars. In our model, a massive protoplanet interrupts the flow of the outer dust-rich disc on its protostar, and at the same time looses a part of its dust-poor envelope into the inner disc. This then powers the observed gas-but-no-dust accretion onto the star. Upon a more detailed investigation, we find that this scenario is quite natural for young massive discs but is less so for older discs, e.g., those whose self-gravitating phase has terminated a fraction of a Million year or more ago. This stems from the fact that TD protoplanets of such an age should have contracted significantly, and so are unlikely to loose much mass. Therefore, we conclude that either (i) the population of "transition discs" with large holes and dust-poor accretion is much younger than generally believed; or (ii) there is a poorly understood stage for late removal of dust-poor envelopes from TD planets; (iii) another explanation for the observations is correct.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

↑