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COSMIC-RAY NEON, WOLF-RAYET STARS, AND THE SUPERBUBBLE ORIGIN OF GALACTIC COSMIC RAYS

机译:宇宙射线氖,狼星和星系宇宙射线的可爆发起源

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We report the abundances of neon isotopes in the Galactic cosmic rays (GCRs) using data from the Cosmic Ray Isotope Spectrometer (CRIS) aboard the Advanced Composition Explorer (ACE). These abundances have been measured for seven energy intervals over the energy range of 84 ≤ E/M ≤ 273 MeV nucleon~(-1). We have derived the ~(22)Ne/~(20)Ne ratio at the cosmic-ray source using the measured ~(21)Ne, ~(19)F, and ~(17)O abundances as "tracers" of secondary production of the neon isotopes. Using this approach, the ~(22)Ne/~(20)Ne abundance ratio that we obtain for the cosmic-ray source is 0.387 ± 0.007(statistical) ± 0.022(systematic). This corresponds to an enhancement by a factor of 5.3 ± 0.3 over the ~(22)Ne/~(20)Ne ratio in the solar wind. This cosmic-ray source ~(22)Ne/~(20)Ne ratio is also significantly larger than that found in anomalous cosmic rays, solar energetic particles, most meteoritic samples of matter, and interplanetary dust particles. We compare our ACE CRIS data for neon and refractory isotope ratios, and data from other experiments, with recent results from two-component Wolf-Rayet (W-R) models. The three largest deviations of GCR isotope ratios from solar system ratios predicted by these models, ~(12)C/~(16)O, ~(22)Ne/~(20)Ne, and ~(58)Fe/~(56)Fe, are indeed present in the GCRs. In fact, all of the isotope ratios that we have measured are consistent with a GCR source consisting of about 80% material with solar system composition and about 20% W-R material. Since W-R stars are evolutionary products of OB stars, and most OB stars exist in OB associations that form superbubbles, the good agreement of these data with W-R models suggests that superbubbles are the likely source of at least a substantial fraction of GCRs.
机译:我们使用先进成分浏览器(ACE)上宇宙射线同位素光谱仪(CRIS)的数据报告银河宇宙射线(GCR)中氖同位素的丰度。在84≤E / M≤273 MeV核仁〜(-1)的能量范围内,已针对七个能量间隔测量了这些丰度。我们使用测得的〜(21)Ne,〜(19)F和〜(17)O丰度作为次级的“示踪物”,得出了宇宙射线源处的〜(22)Ne /〜(20)Ne比。氖同位素的产生。使用这种方法,我们获得的宇宙射线源〜(22)Ne /〜(20)Ne丰度比为0.387±0.007(统计值)±0.022(系统值)。这对应于太阳风中〜(22)Ne /〜(20)Ne比提高5.3±0.3倍。宇宙射线源〜(22)Ne /〜(20)Ne之比也明显大于异常宇宙射线,太阳高能粒子,大多数气象样品和行星际尘埃粒子中发现的比率。我们比较了ACE CRIS数据的氖和难熔同位素比率,以及其他实验的数据,以及二组分Wolf-Rayet(W-R)模型的最新结果。这些模型预测的GCR同位素比与太阳系比的三个最大偏差为〜(12)C /〜(16)O,〜(22)Ne /〜(20)Ne和〜(58)Fe /〜( 56)铁确实存在于GCR中。实际上,我们测量的所有同位素比率均与GCR来源一致,该来源由约80%的具有太阳系组成的材料和约20%的W-R材料组成。由于W-R恒星是OB恒星的演化产物,并且大多数OB恒星存在于形成超气泡的OB关联中,因此这些数据与W-R模型的良好一致性表明,超气泡是至少大部分GCR的可能来源。

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