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Presolar SiC Grains of Type A and B: Their Isotopic Compositions and Stellar Origins

机译:A型和B型太阳前SiC晶粒的同位素组成和恒星起源

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A total of 124 presolar SiC grains of type A and B (defined as having 12C/13C 10) were identified by ion imaging in an acid-resistant residue of the Murchison carbonaceous meteorite. Their isotopic ratios, together with those of 28 previously analyzed A+B grains, are reported here. The 14N/15N ratios range from 39 to 104, with one-third of the grains having 14N/15N ratios lower than the solar value of 272. Inferred 26Al/27Al ratios of A+B grains range up to 10-2. These isotopic compositions clearly distinguish A+B grains from other presolar SiC populations. Among the A+B grains, grains with lower 12C/13C ratios tend to have lower 14N/15N and higher 26Al/27Al ratios. Silicon of A+B grains is enriched in the neutron-rich isotopes (29Si/28Si up to 1.20 times solar, 30Si/28Si up to 1.13 times solar), and in an Si three-isotope plot the distribution of the isotopic ratios is very similar to that of mainstream grains, indicating that the parent stars of the A+B grains had close-to-solar metallicity. Titanium isotopic ratios of 13 grains, out of 30 analyzed, deviate from solar by more than 2 σ in at least one isotopic ratio and span the same range as those of mainstream grains. Trace element abundance patterns of 20 previously measured A+B grains indicate that seven condensed from an atmosphere without s-process enrichments, while 13 did so from an atmosphere enriched in s-process elements by 3-5 times solar. Observationally, the most likely sources of A+B grains with solar s-process abundances are J-type carbon stars, but the origin of these stars is unclear. Born-again asymptotic giant branch (AGB) stars, typified by Sakurai's object (V4334 Sgr), are possible sources of A+B grains with enhanced s-process elemental abundances. Other C-rich stars with low 12C/13C ratios including R stars and CH stars are less likely stellar sources. Whatever the stellar sources, both H and He burning as well as mixing must have occurred in the proper combination to produce both low 12C/13C ratios and C O in the envelope. A special nucleosynthetic problem is posed by the 14N/15N ratios of the grains. High ratios can be explained by hot bottom burning and by cool bottom processing in thermally pulsing AGB stars. Another proposed scenario that possibly yields this signature is extensive mixing of He-burning material into the H-rich envelope during the core He flash. However, the spread of the 14N/15N ratios and lower-than-solar 14N/15N ratios remains unexplained. The isotopic and elemental compositions of A+B grains can provide new information about nucleosynthesis in their possible parent stars that cannot be obtained in any other way.
机译:通过离子成像在Murchison碳质陨石的耐酸残渣中鉴定出总共124个A型和B型(定义为12C / 13C <10)的太阳前SiC晶粒。此处报告了它们的同位素比率,以及先前分析的28种A + B颗粒的同位素比率。 14N / 15N比在39至104范围内,其中三分之一的14N / 15N比值比272的太阳光值低。推断出的A + B晶粒的26Al / 27Al比值范围最大为10-2。这些同位素组成清楚地将A + B晶粒与其他太阳前SiC种群区分开。在A + B晶粒中,具有较低的12C / 13C比率的晶粒倾向于具有较低的14N / 15N和较高的26Al / 27Al比率。 A + B晶粒中的硅富含富含中子的同位素(29Si / 28Si可达太阳的1.20倍,30Si / 28Si可达太阳的1.13倍),并且在Si三同位素图中,同位素比率的分布非常与主流晶粒相似,表明A + B晶粒的母星具有接近太阳能的金属性。在分析的30种晶粒中,13种晶粒的钛同位素比率至少以一种同位素比率偏离太阳2σ以上,并且与主流晶粒的范围相同。先前测得的20种A + B晶粒的痕量元素丰度图表明,有7种元素是从没有进行S加工富集的大气中凝结的,而有13种是从富含s过程元素的大气中以太阳的3-5倍冷凝的。观察到,具有太阳S过程丰度的A + B晶粒最可能的来源是J型碳星,但这些星的起源尚不清楚。以樱井天体(V4334 Sgr)为代表的重生渐近巨型分支(AGB)星,可能是具有增强的S-过程元素丰度的A + B晶粒的来源。其他具有低12C / 13C比的富C恒星,包括R恒星和CH恒星,不太可能是恒星源。无论是哪种恒星源,都必须以适当的组合进行H和He燃烧以及混合,以在外壳中产生低的12C / 13C比和C>O。晶粒的14N / 15N比构成了一个特殊的核合成问题。高比率可以通过热底部燃烧和热脉冲AGB星中的底部冷却处理来解释。另一个可能产生此特征的建议方案是在核心He闪光期间将He燃烧的材料广泛混合到富H的包膜中。但是,尚无法解释14N / 15N比和低于太阳的14N / 15N比的分布。 A + B颗粒的同位素和元素组成可以提供有关其可能的母星中核合成的新信息,而其他任何方式都无法获得。

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