论文标题
根据SDSS/Apogee
The Chemical Compositions of Accreted and {\it in situ} Galactic Globular Clusters According to SDSS/APOGEE
论文作者
论文摘要
银河球状簇(GCS)的运动学和化学组成的研究使星系的恒星形成,化学演化和质量组装的历史可以重建。使用SDSS/Apogee调查的最新数据发布(DR16),我们确定了3,090颗与46个GC相关的恒星。使用先前定义的运动学关联,我们将样品分解为八个单独的组,并检查基于运动学的分类图如何在化学组成空间中,仅考虑$α$(主要是SI和MG)元素和FE。我们的结果表明:(i)化学空间中原位和积聚亚组的基因座匹配其田间对应物的基因群; (ii)来自不同单个积累亚组的GC在化学空间中占据了相同的基因座。这可能意味着它们具有相似的起源,或者与经历了类似化学富集历史的不同卫星相关。 (iii)与Massari和合作者定义的低轨道能亚组相关的GC的化学组成与原位起源广泛一致。但是,在低金属端,积聚和原位种群之间的区别被模糊了。 (iv)关于其起源模棱两可的GC的状态,我们得出以下结论:Si-Fe平面中的位置表明Liller 1的原位起源是NGC 5904和NGC 6388。
Studies of the kinematics and chemical compositions of Galactic globular clusters (GCs) enable the reconstruction of the history of star formation, chemical evolution, and mass assembly of the Galaxy. Using the latest data release (DR16) of the SDSS/APOGEE survey, we identify 3,090 stars associated with 46 GCs. Using a previously defined kinematic association, we break the sample down into eight separate groups and examine how the kinematics-based classification maps into chemical composition space, considering only $α$ (mostly Si and Mg) elements and Fe. Our results show that: (i) The loci of both in situ and accreted subgroups in chemical space match those of their field counterparts; (ii) GCs from different individual accreted subgroups occupy the same locus in chemical space. This could either mean that they share a similar origin or that they are associated with distinct satellites which underwent similar chemical enrichment histories; (iii) The chemical compositions of the GCs associated with the low orbital energy subgroup defined by Massari and collaborators is broadly consistent with an in situ origin. However, at the low metallicity end, the distinction between accreted and in situ populations is blurred; (iv) Regarding the status of GCs whose origin is ambiguous, we conclude the following: the position in Si-Fe plane suggests an in situ}origin for Liller 1 and a likely accreted origin for NGC 5904 and NGC 6388. The case of NGC 288 is unclear, as its orbital properties suggest an accretion origin, its chemical composition suggests it may have formed in situ.