arXivDaily arXiv每日学术速递 周一至周五更新
arXiv 2504.08042astro-ph.EPastro-ph.SR
收藏

磁化原行星盘温度结构的长期演化及其对行星组成二分性的启示

Long-term evolution of the temperature structure in magnetized protoplanetary disks and its implication for the dichotomy of planetary composition

Shoji Mori, Masanobu Kunitomo, Masahiro Ogihara

AI总结:

本研究通过模拟磁化层流原行星盘的长期热演化,结合最新吸积加热认知与风致质量损失,揭示了吸积加热的空间分布规律,并解释了1-10地球质量行星的水含量二分性成因。

摘要:

原行星盘的热结构与演化对行星形成起着至关重要的作用。除恒星辐照外,吸积加热也被认为会显著影响原行星盘的热结构与行星形成过程。我们展示了层流磁化原行星盘热结构的长期演化(从II类阶段初期到原行星盘消散),以探究吸积加热在何时何地成为主导热源。此外,我们还证明了原行星盘结构的差异会影响正在形成的行星的水含量。我们考虑了由磁流体动力学(MHD,磁流体动力学)和光致蒸发原行星盘风导致的质量损失,以研究风致质量损失对吸积率分布的影响。我们的模型纳入了对吸积加热的最新认知,即层流原行星盘中的吸积加热效率低于湍流原行星盘,因为加热发生在光学厚度更薄的高度,且能量会被原行星盘风带走。我们发现,即使在II类阶段早期的原行星盘中,1-10天文单位(au)处的吸积加热也弱于辐照加热,但它可以影响内1 au区域的温度。我们还发现,与外区相比,内区的磁流体动力学风致质量损失可显著降低吸积率,进而减弱吸积加热。此外,利用演化中的原行星盘结构,我们证明了当吸积加热模型更新时,原行星的演化会受到影响。特别是,我们发现我们的模型产生了质量为1-10 $M_\bigoplus$(地球质量)的行星水含量二分性。

英文摘要:

The thermal structure and evolution of protoplanetary disks play a crucial role in planet formation. In addition to stellar irradiation, accretion heating is also thought to significantly affect the disk thermal structure and planet formation processes. We present the long-term evolution (from the beginning of Class II to disk dissipation) of thermal structures in laminar magnetized disks to investigate where and when accretion heating is a dominant heat source. In addition, we demonstrate that the difference in the disk structures affects the water content of forming planets. We considered the mass loss by magnetohydrodynamic (MHD) and photoevaporative disk winds to investigate the influence of wind mass loss on the accretion rate profile. Our model includes the recent understanding of accretion heating, that is, accretion heating in laminar disks is less efficient than that in turbulent disks because the surface is heated at optically thinner altitudes and energy is removed by disk winds. We find that accretion heating is weaker than irradiation heating at about 1--10 au even in the early Class II disk, but it can affect the temperature in the inner 1 au region. We also find that the magnetohydrodynamic wind mass loss in the inner region can significantly reduce the accretion rate compared with the rate in the outer region, which in turn reduces accretion heating. Furthermore, using evolving disk structures, we demonstrate that when accretion heating models are updated, the evolution of protoplanets is affected. In particular, we find that our model produces a dichotomy of the planetary water fraction of 1--10 $M_\oplus$.

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。

↑