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HIGH-CONTRAST IMAGING SEARCH FOR PLANETS AND BROWN DWARFS AROUND THE MOST MASSIVE STARS IN THE SOLAR NEIGHBORHOOD*

机译:太阳近邻中大部分质量恒星周围的行星和褐矮星的高对比度成像搜索*

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There has been a long-standing discussion in the literature as to whether core accretion or disk instability is the dominant mode of planet formation. Over the last decade, several lines of evidence have been presented showing that core accretion is most likely the dominant mechanism for the close-in population of planets probed by radial velocity and transits. However, this does not by itself prove that core accretion is the dominant mode for the total planet population, since disk instability might conceivably produce and retain large numbers of planets in the far-out regions of the disk. If this is a relevant scenario, then the outer massive disks of B-stars should be among the best places for massive planets and brown dwarfs to form and reside. In this study, we present high-contrast imaging of 18 nearby massive stars of which 15 are in the B2-A0 spectral-type range and provide excellent sensitivity to wide companions. By comparing our sensitivities to model predictions of disk instability based on physical criteria for fragmentation and cooling, and using Monte Carlo simulations for orbital distributions, we find that ~85% of such companions should have been detected in our images on average. Given this high degree of completeness, stringent statistical limits can be set from the null-detection result, even with the limited sample size. We find that 30% of massive stars form and retain disk instability planets, brown dwarfs, and very low mass stars of 100 M jup within 300?AU, at 99% confidence. These results, combined with previous findings in the literature, lead to the conclusion that core accretion is likely the dominant mode of planet formation.
机译:关于堆芯或盘的不稳定性是行星形成的主要方式,文献中进行了长期的讨论。在过去的十年中,已经提出了几条证据,表明通过径向速度和过境探测,岩心积聚最有可能是近距离行星种群的主要机制。但是,这本身并不能证明核心增长是整个行星总数的主要模式,因为可以想象,磁盘不稳定会在磁盘的较远区域产生并保留大量行星。如果这是一个合适的场景,那么B恒星的外层大质量盘应该是形成大质量行星和褐矮星并形成和居住的最佳场所之一。在这项研究中,我们提出了18个附近大质量恒星的高对比度成像,其中15个处于B2-A0光谱类型范围,并且对宽伴星具有出色的灵敏度。通过将敏感性与基于碎片和冷却的物理准则的磁盘不稳定性的模型预测进行比较,并使用蒙特卡洛模拟进行轨道分布,我们发现平均应该在我们的图像中检测到此类伴星的〜85%。鉴于这种高度的完整性,即使样本量有限,也可以根据无效检测结果设置严格的统计极限。我们发现,在300?AU以内,<30%的大质量恒星形成并保留了磁盘不稳定的行星,褐矮星和质量小于100M的低质量恒星,且置信度为99%。这些结果与文献中的先前发现相结合得出结论,即岩心积聚可能是行星形成的主要方式。

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