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Insights into Planet Formation from Debris Disks II. Giant Impacts in Extrasolar Planetary Systems

机译:碎片盘II对行星形成的见解。太阳系外行星系统的巨大影响

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Giant impacts refer to collisions between two objects each of which is massive enough to be considered at least a planetary embryo. The putative collision suffered by the proto-Earth that created the Moon is a prime example, though most Solar System bodies bear signatures of such collisions. Current planet formation models predict that an epoch of giant impacts may be inevitable, and observations of debris around other stars are providing mounting evidence that giant impacts feature in the evolution of many planetary systems. This chapter reviews giant impacts, focussing on what we can learn about planet formation by studying debris around other stars. Giant impact debris evolves through mutual collisions and dynamical interactions with planets. General aspects of this evolution are outlined, noting the importance of the collision-point geometry. The detectability of the debris is discussed using the example of the Moon-forming impact. Such debris could be detectable around another star up to 10 Myr post-impact, but model uncertainties could reduce detectability to a few 100 yr window. Nevertheless the 3 % of young stars with debris at levels expected during terrestrial planet formation provide valuable constraints on formation models; implications for super-Earth formation are also discussed. Variability recently observed in some bright disks promises to illuminate the evolution during the earliest phases when vapour condensates may be optically thick and acutely affected by the collision-point geometry. The outer reaches of planetary systems may also exhibit signatures of giant impacts, such as the clumpy debris structures seen around some stars.
机译:巨大撞击是指两个物体之间的碰撞,每个物体的质量足以视为至少一个行星胚胎。尽管大多数太阳系天体都具有这种碰撞的特征,但创建地球的原始地球遭受的推定碰撞是一个典型的例子。当前的行星形成模型预测,巨大撞击的时代可能是不可避免的,对其他恒星周围碎片的观察也提供了越来越多的证据,表明许多行星系统的演化都具有巨大撞击的特征。本章回顾了巨大的影响,重点介绍了我们可以通过研究其他恒星周围的碎片来了解有关行星形成的知识。巨大的撞击碎片通过与行星的相互碰撞和动力相互作用而演化。概述了这种演变的一般方面,并指出了碰撞点几何的重要性。以形成月球的撞击为例,讨论了碎片的可检测性。这样的碎片可以在撞击后高达10 Myr的另一颗恒星周围被探测到,但是模型的不确定性可能会将可探测性降低到100年窗口。然而,有3%的年轻恒星的碎片在地球行星形成过程中的预期水平上提供了对形成模型的宝贵约束;还讨论了超地球形成的意义。最近在某些亮盘上观察到的变化有望阐明最早阶段的演变,此时蒸汽凝结物可能在光学上很厚,并且受碰撞点几何形状的影响很大。行星系统的外围也可能显示出巨大撞击的迹象,例如在某些恒星周围看到的块状碎片结构。

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