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arXiv 2409.06342astro-ph.EPastro-ph.SR
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原行星盘的形成与演化:结合观测、模拟和宇宙化学约束

Formation and evolution of a protoplanetary disk: combining observations, simulations and cosmochemical constraints

Alessandro Morbidelli, Yves Marrocchi, Adnan Ali Ahmad, Asmita Bhandare, Sebastien Charnoz, Benoit Commercon, Cornellis P. Dullemond, Tristan Guillot, Patrick H… 展开作者

Alessandro Morbidelli, Yves Marrocchi, Adnan Ali Ahmad, Asmita Bhandare, Sebastien Charnoz, Benoit Commercon, Cornellis P. Dullemond, Tristan Guillot, Patrick Hennebelle, Yueh-Ning Lee, Francesco Lovascio, Raphael Marschall, Bernard Marty, Anaelle Maury, Okamoto Tamami

AI总结:

本研究提出一个与宇宙化学约束、观测和模拟兼容的原太阳盘演化模型,指出其演化过程典型,太阳系独特性源于行星形成的混沌本质。

摘要:

我们提出了一个关于原太阳盘演化的合理且连贯的观点,该观点与宇宙化学约束相一致,并与其他原行星盘的观测结果及复杂的数值模拟相兼容。高温凝聚物(CAIs和AOAs)在原太阳附近形成后被传输到外盘的证据,可以通过以下两种方式解释:要么是原行星盘早期阶段的剧烈径向扩散,要么是这些凝聚物通过原恒星外流从原太阳附近快速传输到大盘半径处。假设在吸积阶段末期吸积的物质在同位素上具有明显特征,这使我们能够解释陨石中观测到的核合成同位素异常的二分法,并对彗星中难熔元素的同位素组成提出了引人注目的预测。当物质吸积减弱时,原行星盘开始作为吸积盘演化。最初,尘埃向内漂移,使尘埃成分的半径缩小至约45 au,大约是气体成分宽度的1/2。随后必须出现了某些结构,在盘中产生了一系列压力极大值,将尘埃在百万年(Myr)时间尺度上捕获。这使得小行星体能够在截然不同的时间形成,而同位素性质没有显著变化。没有物质通过流纹(streamers)晚期吸积到盘上。正如陨石中的古地磁数据所示,盘在大约5百万年内消失。总之,原太阳盘的演化在尺寸、寿命和尘埃行为方面似乎相当典型,这表明太阳系相对于系外行星系统的独特性可能源于行星形成的混沌本质,而非母盘层面的差异。

英文摘要:

We present a plausible and coherent view of the evolution of the protosolar disk that is consistent with the cosmochemical constraints and compatible with observations of other protoplanetary disks and sophisticated numerical simulations. The evidence that high-temperature condensates, CAIs and AOAs, formed near the protosun before being transported to the outer disk can be explained by either an early phase of vigorous radial spreading of the disk, or fast transport of these condensates from the vicinity of the protosun towards large disk radii via the protostellar outflow. The assumption that the material accreted towards the end of the infall phase was isotopically distinct allows us to explain the observed dichotomy in nucleosynthetic isotopic anomalies of meteorites and leads to intriguing predictions on the isotopic composition of refractory elements in comets. When the infall of material waned, the disk started to evolve as an accretion disk. Initially, dust drifted inwards, shrinking the radius of the dust component to ~ 45 au, probably about 1/2 of the width of the gas component. Then structures must have emerged, producing a series of pressure maxima in the disk which trapped the dust on My timescales. This allowed planetesimals to form at radically distinct times without changing significantly of isotopic properties. There was no late accretion of material onto the disk via streamers. The disk disappeared in ~5 Myr, as indicated by paleomagnetic data in meteorites. In conclusion, the evolution of the protosolar disk seems to have been quite typical in terms of size, lifetime, and dust behavior, suggesting that the peculiarities of the Solar system with respect to extrasolar planetary system probably originate from the chaotic nature of planet formation and not at the level of the parental disk.

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