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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Fe–Ni and Al–Mg isotope records in UOC chondrules: Plausible stellar source of ~(60)Fe and other short-lived nuclides in the early Solar System
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Fe–Ni and Al–Mg isotope records in UOC chondrules: Plausible stellar source of ~(60)Fe and other short-lived nuclides in the early Solar System

机译:UOC球体中的Fe–Ni和Al–Mg同位素记录:早期太阳系中〜(60)Fe和其他短寿命核素的可能星源

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摘要

The short-lived now-extinct nuclide ~(60)Fe, present in the early Solar System, is a unique product of stellar nucleosynthesis. Even though the first hint for its presence in the early Solar System was obtained more than two decades back, a robust value for Solar System initial (SSI) ~(60)Fe/~(56)Fe is yet to be established. A combined study of ~(26)Al–~(26)Mg and ~(60)Fe–~(60)Ni isotope systematics in chondrules from unequilibrated ordinary chondrites of low petrologic type, Semarkona (LL3.0), LEW 86134 (L3.0), and Y 791324 (L3.1), has been conducted to infer the value of SSI ~(60)Fe/~(56)Fe. Seven of the analysed chondrules host resolved radiogenic excess in both ~(60)Ni and ~(26)Mg resulting from in situ decay of the short-lived nuclides ~(60)Fe and ~(26)Al, respectively. The initial ~(26)Al/~(27)Al values for these chondrules range from (6.9 ± 5.8) × 10~(-6) to (3.01 ± 1.78) × 10~(-5) that suggest their formation between 2.1 and 0.6 Ma after CAIs. The initial ~(60)Fe/~(56)Fe at the time of formation of these chondrules ranges from (3.2 ± 1.3) × 10~(-7) to (1.12 ± 0.39) × 10~(-6) and show a good correlation with their initial ~(26)Al/~(27)Al values suggesting co-injection of the two short-lived nuclides, ~(60)Fe and ~(26)Al, into the protosolar cloud from the same stellar source. Considering ~(26)Al as a reliable early Solar System chronometer, this data set yield a SSI ~(60)Fe/~(56)Fe value of (7.0 ± 1.2) × 10~(-7), if we adopt a half-life value of 2.6 Ma for ~(60)Fe reported in a recent study. Model stellar nucleosynthesis yields suggest that both a high mass (5–6.5 M_⊙) Asymptotic Giant Branch (AGB) star or a supernova (SN) could be the source of ~(60)Fe and ~(26)Al present in the early Solar System. A high mass (~25M_⊙) SN appears more plausible because of the much higher probability of its close association with the protosolar molecular cloud than a high mass AGB star. Such a SN can also account for SSI abundance of ~(26)Al and its correlated presence with ~(60)Fe in chondrules.
机译:存在于早期太阳系中的寿命短,现已灭绝的核素〜(60)Fe是恒星核合成的独特产物。尽管早在二十多年前就获得了有关其在早期太阳系中存在的第一个提示,但尚未确定太阳系初始(SSI)〜(60)Fe /〜(56)Fe的可靠值。低岩石学类型非平衡普通球粒陨石中的〜(26)Al–〜(26)Mg和〜(60)Fe–〜(60)Ni同位素系统的组合研究,Semarkona(LL3.0),LEW 86134( L3.0)和Y 791324(L3.1)已被用来推断SSI〜(60)Fe /〜(56)Fe的值。被分析的七种球藻宿主分别解析了〜(60)Ni和〜(26)Mg的放射源过量,这分别是由短寿命核素〜(60)Fe和〜(26)Al的原位衰减引起的。这些软骨的初始〜(26)Al /〜(27)Al值介于(6.9±5.8)×10〜(-6)至(3.01±1.78)×10〜(-5)之间,表明它们在2.1之间形成CAI后为0.6 Ma。这些球粒形成时的初始〜(60)Fe /〜(56)Fe范围为(3.2±1.3)×10〜(-7)至(1.12±0.39)×10〜(-6)并显示与它们的初始〜(26)Al /〜(27)Al值具有良好的相关性,表明两个短寿命核素〜(60)Fe和〜(26)Al从同一恒星共同注入原生质云中资源。如果将〜(26)Al作为可靠的早期太阳系天文钟,则如果采用以下公式,则该数据集的SSI〜(60)Fe /〜(56)Fe值为(7.0±1.2)×10〜(-7)。在最近的研究中报道了〜(60)Fe的半衰期值为2.6 Ma。模型恒星的核合成结果表明,在早期,高质量(5–6.5M_⊙)渐近巨枝(AGB)星或超新星(SN)可能都是〜(60)Fe和〜(26)Al的来源太阳系。高质量(〜25M_⊙)SN似乎更合理,因为与高质量AGB恒星相比,其与原生质分子云紧密结合的可能性要高得多。这样的SN也可以解释〜(26)Al的SSI丰度及其与软骨中〜(60)Fe的相关存在。

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