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Stellar Metallicity and Planet Formation

机译:恒星金属和行星形成

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We describe results from two independent analyses of the [Fe/H]abundance of stars in two separate planet search programs. For the Keck, AAT,and Lick (KAL) planet search program, we determined stellar parameters spectroscopically.Results for the CORALIE and KAL both show a similar steep increase in the fraction of stars with known planets as stellar [Fe/H] increase.This planet metallicity correlation is a key observational constraint on the formation and evolution of giant planets. We rule out changes in velocity precision as the cause of the correlation. By comparing stars with different convection zone depths (along and off the main-sequence), we rule out chemical enrichment by accretion as the origin of the correlation. Most known planets have migrated inwards since formation. The end point of migration does not depend on stellar [Fe/H], but it is still possible that migration occurs only above some metallicity threshold. The planet-metallicity correlation is consistent with core-accretion scenarios of giant planet formation.
机译:我们描述了两种独立分析的两种独立分析的恒星在两个单独的行星搜索程序中的恒星。对于Keck,AAT和Lick(kal)行星搜索程序,我们确定了恒星参数的光谱参数。对于Coralie和Kal的结果表明,具有已知行星的恒星分数与恒星[Fe / h]增加相似的陡峭增加。该行星金属性相关是对巨大行星形成和演化的关键观测限制。我们排除了速度精度的变化作为相关性的原因。通过将恒星与不同的对流区深度进行比较(沿着主序列),我们将化学富集作为相关性的来源。最着名的行星自形成以来已向内迁移。迁移的终点不依赖于恒星[Fe / h],但仍然可能仅在一些金属性阈值高于之上发生迁移。地球金属性相关性与巨大行星形成的核心增值情景一致。

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