论文标题

将行星胚的形成与行星形成I:地球表面密度在陆地行星区域的影响

Linking planetary embryo formation to planetesimal formation I: The impact of the planetesimal surface density in the terrestrial planet zone

论文作者

Voelkel, Oliver, Deienno, Rogerio, Kretke, Katherine, Klahr, Hubert

论文摘要

行星胚胎的增长时间尺度及其形成过程对于我们对行星系统如何形成和发展的理解至关重要。他们确定了在脉络膜磁盘生命阶段的后续生长机制。我们通过碰撞生长和动态形成100公里大小的行星模具的碎片来量化行星胚胎的时间尺度和空间分布。在我们的研究中,粘性磁盘进化和行星形成的形成时间尺度与陆地行星区域的行星胚胎的形成有关。我们将粘性气体演化,灰尘和卵石动力学以及卵石通量调节的行星形成连接到n体代码Lipad。我们的框架使我们能够研究粘性磁盘的首百万年,直径为100 km的行星尺寸的形成,生长,碎片和演变。我们的研究显示了行星表面密度演化对行星胚胎形成的优先位置和时间尺度的影响。提出了基于局部行星表面密度演化的胚胎形成的一维分析模型。该模型设法以N体模拟的计算成本的一小部分来重现空间分布,形成速率和行星胚胎总数。陆地行星区域中行星胚胎的形成同时发生与行星的形成。寡头制度中行星胚胎的局部行星表面密度演化和轨道间距很好地充当模型的行星胚胎形成的限制。我们的胚胎形成模型将是关于行星形成的未来研究的宝贵资产。

The growth time scales of planetary embryos and their formation process are imperative for our understanding on how planetary systems form and develop. They determine the subsequent growth mechanisms during the life stages of a circumstellar disk. We quantify the timescales and spatial distribution of planetary embryos via collisional growth and fragmentation of dynamically forming 100km sized planetesimals. In our study, the formation timescales of viscous disk evolution and planetesimal formation are linked to the formation of planetary embryos in the terrestrial planet zone. We connect a one dimensional model for viscous gas evolution, dust and pebble dynamics and pebble flux regulated planetesimal formation to the N-body code LIPAD. Our framework enables us to study the formation, growth, fragmentation and evolution of planetesimals with an initial size of 100km in diameter for the first million years of a viscous disk. Our study shows the effect of the planetesimal surface density evolution on the preferential location and timescales of planetary embryo formation. A one dimensional analytically derived model for embryo formation based on the local planetesimal surface density evolution is presented. This model manages to reproduce the spatial distribution, formation rate and total number of planetary embryos at a fraction of the computational cost of the N-body simulations. The formation of planetary embryos in the terrestrial planet zone occurs simultaneously to the formation of planetesimals. The local planetesimal surface density evolution and the orbital spacing of planetary embryos in the oligarchic regime serve well as constraints to model planetary embryo formation analytically. Our embryo formation model will be a valuable asset in future studies regarding planet formation.

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