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行星加热阻止了行星内核的向内迁移。

Planet heating prevents inward migration of planetary cores.

机构信息

IATE, Observatorio Astronómico, Universidad Nacional de Córdoba, Laprida 854, Córdoba, X5000BGR, Argentina.

Instituto de Ciencias Físicas, Universidad Nacional Autónoma de México, Avenidad Universidad s/n, 62210 Cuernavaca, Morelos, Mexico.

出版信息

Nature. 2015 Apr 2;520(7545):63-5. doi: 10.1038/nature14277.

Abstract

Planetary systems are born in the disks of gas, dust and rocky fragments that surround newly formed stars. Solid content assembles into ever-larger rocky fragments that eventually become planetary embryos. These then continue their growth by accreting leftover material in the disk. Concurrently, tidal effects in the disk cause a radial drift in the embryo orbits, a process known as migration. Fast inward migration is predicted by theory for embryos smaller than three to five Earth masses. With only inward migration, these embryos can only rarely become giant planets located at Earth's distance from the Sun and beyond, in contrast with observations. Here we report that asymmetries in the temperature rise associated with accreting infalling material produce a force (which gives rise to an effect that we call 'heating torque') that counteracts inward migration. This provides a channel for the formation of giant planets and also explains the strong planet-metallicity correlation found between the incidence of giant planets and the heavy-element abundance of the host stars.

摘要

行星系统诞生于环绕新形成恒星的气体、尘埃和岩石碎片盘中。固体物质聚集形成越来越大的岩石碎片,最终成为行星胚胎。然后,它们通过在盘中吸积残留物质继续生长。与此同时,盘中的潮汐效应导致胚胎轨道发生径向漂移,这一过程称为迁移。理论预测,对于小于三到五个地球质量的胚胎,会发生快速向内迁移。仅通过向内迁移,这些胚胎很少能成为位于地球到太阳距离以内和以外的巨行星,这与观测结果形成对比。在这里,我们报告说,与吸积下落物质相关的温度升高的不对称性会产生一种力(这会产生一种我们称之为“加热扭矩”的效应),这种力会抵消向内迁移。这为巨行星的形成提供了一个渠道,也解释了在巨行星的出现率和主星重元素丰度之间发现的强烈的行星-金属丰度相关性。

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