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arXiv 2510.07428astro-ph.EP
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有风原行星盘中行星开凿间隙处的增强卵石漂移

Enhanced Pebble Drift Across Planet-Opened Gaps in Windy Protoplanetary Disks

Lorraine Nicholson, Jaehan Bae

AI总结:

本研究通过二维多流体模拟发现,磁驱动风能增强卵石漂移,使毫米级颗粒穿透巨行星开凿的间隙,从而影响内盘行星形成。

摘要:

当一颗巨行星在原行星盘中形成时,它会在其轨道周围刻出一个间隙,将盘分为两部分:内盘和外盘。传统的盘吸积模型假设物质输运由黏性驱动,这些模型揭示出行星诱导的间隙像一个过滤器,阻止大尘埃颗粒流入内盘。然而,越来越多的证据表明,物质输运可能由磁驱动风主导。通过开展一系列二维多流体流体动力学模拟,其中风以参数化模型实现,我们探索了在气体吸积由磁驱动风主导的盘中,尘埃过滤效率以及被过滤尘埃颗粒尺寸如何变化。我们发现,由风驱动的向内气体流能够使尘埃克服外间隙边缘的压力凸起,并穿透行星诱导的间隙。能够穿透间隙的尘埃颗粒最大尺寸随风强度增加而增大。值得注意的是,我们发现当风很强(质量损失率 = 1e-7 太阳质量/年)时,毫米大小的颗粒能够穿透由多个木星质量行星打开的间隙。我们的结果表明,磁驱动风可以显著增强卵石漂移,并影响内原行星盘中的行星形成。

英文摘要:

When a giant planet forms in a protoplanetary disks, it carves a gap around its orbit separating the disk into two parts: inner disk and outer disk. Traditional disk accretion models, which assume material transport is driven by viscosity, reveal that the planet-induced gap acts like a filter which blocks large dust grains from flowing into the inner disk. However, there is growing evidence that material transport may be driven by magnetically-driven winds instead. By carrying out a suite of two-dimensional multi-fluid hydrodynamic simulations where wind is implemented with a parameterized model, we explored how dust filtration efficiency and the size of dust grains filtered change in disks where gas accretion is dominated by magnetically-driven winds. We found that the inward gas flow driven by the wind can enable dust to overcome the pressure bump at the outer gap edge and penetrate the planet-induced gap. The maximum size of dust grains capable of penetrating the gap increasing with the wind strength. Notably, we found that when wind is strong (mass loss rate = 1e-7 M_sun/yr), mm-sized grains can penetrate the gap opened by a multi-Jovian-mass planet. Our results suggest that magnetically driven winds can significantly enhance pebble drift and impact planet formation in the inner protoplanetary disk.

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。

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