论文标题

在锂6上作为红色巨人锂富集机制的诊断

On Lithium-6 as diagnostic of the lithium-enrichment mechanism in red giants

论文作者

Aguilera-Gómez, Claudia, Chanamé, Julio, Pinsonneault, Marc H.

论文摘要

高锂-7($ \ mathrm {^7li} $)巨人的丰度表示影响恒星的非标准物理过程。可能产生这种签名的机制包括来自外部来源的污染,例如行星,内部生产以及随后的混合到恒星表面。但是,区分不同的解决方案家族已被证明具有挑战性,并且目前没有共识模型可以解释所有数据。锂-6($ \ mathrm {^6li} $)的丰度可能是一种潜在的重要歧视性,因为相对$ \ mathrm {^6li} $和$ \ mathrm {^7li} $ nli} $丰度的丰度预计如果富集来自内部生产或来自内部生产或来自Gulululfment。在这项工作中,我们建模$ \ mathrm {^6li} $和$ \ mathrm {^7li} $在吞噬替代巨人之后的不同巨人。鉴于$ \ mathrm {^6li} $比$ \ mathrm {^7li} $,$ \ mathrm {^6li} $更强烈地影响了银河化学化学演化,在低金属的情况下,在恒星和星球的情况下都低。对于建模的金属([Fe/H] $> -0.5 $),我们使用“最佳情况”初始$ \ mathrm {^6li/^7li} $比率等于太阳值。 $ \ mathrm {^6li} $在吞噬同伴后大幅增加。但是,在靠近太阳能及更高较高的金属上,$ \ mathrm {^6li} $信号在恒星表面不会持续很长时间。因此,在金属富红色巨人中检测表面$ \ mathrm {^6li} $,很可能表明了$ \ mathrm {^6li} $的机制的作用,而不是吞噬行星以外的其他。同时,$ \ mathrm {^6li} $不应用于拒绝$ \ mathrm {^7li} $中吞噬的假设 - 丰富的巨型或支持特定的$ \ mathrm {^7li} $ - 增强机制。

High lithium-7 ($\mathrm{^7Li}$) abundances in giants are indicative of non-standard physical processes affecting the star. Mechanisms that could produce this signature include contamination from an external source, such as planets, or internal production and subsequent mixing to the stellar surface. However, distinguishing between different families of solutions has proven challenging, and there is no current consensus model that explains all the data. The lithium-6 ($\mathrm{^6Li}$) abundance may be a potentially important discriminant, as the relative $\mathrm{^6Li}$ and $\mathrm{^7Li}$ abundances are expected to be different if the enrichment were to come from internal production or from engulfment. In this work, we model the $\mathrm{^6Li}$ and $\mathrm{^7Li}$ abundances of different giants after the engulfment of a substellar mass companion. Given that $\mathrm{^6Li}$ is more strongly affected by Galactic chemical evolution than $\mathrm{^7Li}$, $\mathrm{^6Li}$ is not a good discriminant at low metallicities, where it is expected to be low in both star and planet. For modeled metallicities ([Fe/H]$>-0.5$), we use a "best case" initial $\mathrm{^6Li/^7Li}$ ratio equal to the solar value. $\mathrm{^6Li}$ increases significantly after the engulfment of a companion. However, at metallicities close to solar and higher, the $\mathrm{^6Li}$ signal does not last long in the stellar surface. As such, detection of surface $\mathrm{^6Li}$ in metal-rich red giants would most likely indicate the action of a mechanism for $\mathrm{^6Li}$-enrichment other than planet engulfment. At the same time, $\mathrm{^6Li}$ should not be used to reject the hypothesis of engulfment in a $\mathrm{^7Li}$-enriched giant or to support a particular $\mathrm{^7Li}$-enhancement mechanism.

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