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THE INTERSTELLAR RUBIDIUM ISOTOPE RATIO TOWARD ρ OPHIUCHI A

机译:ρOPHIUCHI A的星际R同位素比

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The isotope ratio ~(85)Rb/~(87)Rb places constraints on models of the nucleosynthesis of heavy elements, but there is no precise determination of the ratio for material beyond the solar system. We report the first measurement of the interstellar Rb isotope ratio. Our measurement of the Rb I line at 7800 A for the diffuse gas toward ρ Oph A yields a value of 1.21 +- 0.30 (1 σ) that differs significantly from the meteoritic value of 2.59. The Rb/K elemental abundance ratio for the cloud also is lower than that seen in meteorites. Comparison of the ~(85)Rb/K and ~(87)Rb/K ratios with meteoritic values indicates that the interstellar ~(85)Rb abundance in this direction is lower than the solar system abundance. We attribute the lower abundance to a reduced contribution from the r-process. Interstellar abundances for Kr, Cd, and Sn are consistent with much less r-process synthesis for the solar neighborhood compared to the amount inferred for the solar system.
机译:同位素比〜(85)Rb /〜(87)Rb限制了重元素的核合成模型,但无法精确确定太阳系以外物质的比例。我们报告了星际Rb同位素比的首次测量。我们在7800 A处测量的Rb I线对于朝向ρOph A的扩散气体产生的值为1.21±0.30(1σ),这与2.59的气象值明显不同。云中的Rb / K元素丰度比也比陨石中的低。 〜(85)Rb / K和〜(87)Rb / K比值与气象值的比较表明,星际〜(85)Rb丰度在此方向上低于太阳系丰度。我们将较低的丰度归因于r进程的减少。与推断的太阳系数量相比,Kr,Cd和Sn的星际丰度与太阳邻域的r过程合成少得多。

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