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Nucleosynthesis in Classical Novae and Its Contribution to the Interstellar Medium

机译:经典新星的核合成及其对星际介质的贡献

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Classical novae, explosions that result from thermonuclear runaways (TNRs) on the surfaces of white dwarfs (WDs) accreting hydrogen-rich matter in close binary systems, are sporadically injecting material processed by explosive hydrogen-burning nucleosynthesis into the interstellar medium (ISM). Although novae probable have processed less than ~0.3% of the interstellar matter in the Galaxy, both theoretical and observational evidence suggests that they may be important sources of the nuclides ~7Li, ~(15)N, and ~(17)O, as well as the radioactive isotopes ~(22)Na and ~(26)Al. The latter nuclides are astrophysically important in that they may have been involved in the production of the ~(22)Ne (Ne-E) and ~(26)Mg enrichments identified in meteoritic inclusions, the composition of which is though to be representative of the chemical and mineral contents of the primitive solar nebula. These inclusions may be partially composed of dust condensed in nova outbursts. We review theoretical expectations for the yields of various isotopes in nova outbursts and conclude that any of the heavy isotope anomalies attributable to novae are most likely produced by the approximately 25%-33% of novae the occur in systems containing massive (M_* > 1.2 M_⊙) oxygen-neon-magnesium (ONeMg) WDs. We attempt to place quantitative constraints on the degree to which classical novae participate in the production of chemical anomalies, both in the primitive solar system and on a Galactic scale. Diffuse Galactic γ-ray fluxes provide particularly important clues to and constraints on the ~(22)Na and ~(26)Al yields from novae, Ultraviolet (UV), optical, and infrared (IR) emission-line spectra of classical novae reveal the abundances of some of the gas-phase elements present in the ejecta; recent results are reviewed. We describe how IR observations of novae reveal dust formation and gas-phase line emission and how they distinguish the temporal development of nova explosions on carbon-oxygen (CO) WDs (CO novae) from those on ONeMg WDs (ONeMg or "neon" novae). Recent studies show that the ejecta in some novae can be strongly cooled by near- and mid-IR forbidden-line radiation from highly ionized ("coronal") atomic states. We compare the abundances deduced from recent UV, optical, and IR observations with theoretical predictions, and we suggest that future studies of IR coronal emission lines may provide additional key information. Novae produce only about 0.1% of the Galactic "stardust" (dust condensed in stellar outflows), but IR observations show that it may be some of the more interesting dust. Novae appear capable of producing astrophysical dust of virtually every known chemical and mineral composition. We summarize recent IR observations of the dust of production scenario in novae and argue that neon novae may lead to the formation of dust grains that carry the Ne-E and ~(26)Mg anomalies.
机译:经典新星是由白矮星(WD)的表面上的热核逃逸(TNR)吸收的,在紧密的双星系统中吸收了富氢物质,这些爆炸是将爆炸性氢燃烧核合成处理的材料偶发地注入星际介质(ISM)。尽管新星可能处理了星系中星际物质的约不到0.3%,但理论和观察证据均表明它们可能是核素〜7Li,〜(15)N和〜(17)O的重要来源,例如以及放射性同位素〜(22)Na和〜(26)Al。后一种核素在天体上很重要,因为它们可能参与了在陨石包裹体中鉴定出的〜(22)Ne(Ne-E)和〜(26)Mg富集的产生,尽管其组成可以代表太阳原始星云的化学和矿物质含量。这些夹杂物可能部分由新星爆发时凝结的尘埃组成。我们回顾了对新星爆发中各种同位素的产率的理论预期,并得出结论,归因于新星的任何重度同位素异常最有可能是由大约25%-33%的新星产生的,这种新星发生在含有大量物质的系统中(M_ *> 1.2 M_⊙)氧氖镁(ONeMg)WD。我们试图在原始太阳系和银河系尺度上,对经典新星参与化学异常产生的程度进行定量限制。弥漫性银河γ射线通量为新星产生的〜(22)Na和〜(26)Al产量提供了特别重要的线索和约束条件,经典新星的紫外线(UV),光学和红外(IR)发射谱喷射器中存在的某些气相元素的丰度;最近的结果进行了审查。我们描述了对新星的红外观测如何揭示尘埃形成和气相线发射,以及它们如何区分碳氧(CO)WD(CO新星)和ONeMg WD(ONeMg或“氖”新星)上的新星爆炸的时间发展。 )。最近的研究表明,某些新星中的喷出物可以被来自高度电离(“冠状”)原子态的近红外和中红外禁线辐射强烈冷却。我们将最新的紫外线,光学和红外观测结果与理论预测值相比较,并建议红外冠状发射线的未来研究可能会提供更多关键信息。 Novae仅产生约0.1%的银河“星尘”(星状流出物中凝结的尘埃),但红外观测表明它可能是一些更有趣的尘埃。 Novae似乎能够产生几乎所有已知化学和矿物成分的天体粉尘。我们总结了IR对新星生产过程中的粉尘的最新IR观测结果,并指出霓虹新星可能导致携带Ne-E和〜(26)Mg异常的尘埃颗粒的形成。

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