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Inner Super-Earths, Outer Gas Giants: How Pebble Isolation and Migration Feedback Keep Jupiters Cold

机译:内超级地球,外气巨人:卵石的隔离和迁移反馈如何使木星保持寒冷

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The majority of gas giants (planets of masses 102?M ⊕) are found to reside at distances beyond ~1 au from their host stars. Within 1 au, the planetary population is dominated by super-Earths of 2–20?M ⊕. We show that this dichotomy between inner super-Earths and outer gas giants can be naturally explained should they form in nearly inviscid disks. In laminar disks, a planet can more easily repel disk gas away from its orbit. The feedback torque from the pile-up of gas inside the planet's orbit slows down and eventually halts migration. A pressure bump outside the planet's orbit traps pebbles and solids, starving the core. Gas giants are born cold and stay cold: more massive cores are preferentially formed at larger distances, and they barely migrate under disk feedback. We demonstrate this using two-dimensional hydrodynamical simulations of disk–planet interaction lasting up to 105 years: we track planet migration and pebble accretion until both come to an end by disk feedback. Whether cores undergo runaway gas accretion to become gas giants or not is determined by computing one-dimensional gas accretion models. Our simulations show that in an inviscid minimum mass solar nebula, gas giants do not form inside ~0.5?au, nor can they migrate there while the disk is present. We also explore the dependence on disk mass and find that gas giants form further out in less massive disks.
机译:发现大多数气体巨人(质量为102?M plane的行星)居住在距其宿主恒星约1 au以上的距离。 1 au内,地球人口以2–20?M super的超地球为主。我们表明,如果内部超地球和外部气体巨人形成于几乎无粘性的磁盘中,则可以自然地解释这种二分法。在层状磁盘中,行星可以更轻松地将磁盘气体驱离其轨道。来自行星轨道内部气体堆积的反馈扭矩会减慢速度,并最终阻止迁移。行星轨道外部的压力颠簸捕获了卵石和固体,使核心处于饥饿状态。气体巨人生来就很冷,并且保持寒冷:更重的岩心优先形成于更远的距离,并且在磁盘反馈的作用下它们几乎不会迁移。我们使用持续时间长达105年的磁盘-行星相互作用的二维流体动力学模拟来证明这一点:我们跟踪行星的迁移和卵石的积聚,直到两者都通过磁盘反馈而结束。通过计算一维气体积聚模型来确定岩心是否经历了失控的气体积聚而变成气体巨人。我们的模拟显示,在最小质量的无形太阳星云中,气体巨星不会在〜0.5?au内形成,也不会在存在磁盘的情况下迁移到那里。我们还探索了对磁盘质量的依赖性,发现天然气巨头在质量较小的磁盘中形成了更远的地方。

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