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DETAILED ABUNDANCES OF PLANET-HOSTING WIDE BINARIES. II. HD 80606+HD 80607

机译:泛滥的广域双星的详细信息。二。高清80606+高清80607

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We present a detailed chemical abundance analysis of 15 elements in the planet-hosting wide binary (PHWB) system HD 80606+HD 80607 using Keck/HIRES spectra. As in our previous analysis of the PHWB HD 20782+HD 20781, we presume that these two G5 dwarf stars formed together and therefore had identical primordial abundances. In this binary, HD 80606 hosts an eccentric () giant planet at ~0.5 AU, but HD 80607 has no detected planets. If close-in giant planets on eccentric orbits are efficient at scattering rocky planetary material into their host stars, then HD 80606 should show evidence of having accreted rocky material while HD 80607 should not. Here we show that the trends of abundance versus element condensation temperature for HD 80606 and HD 80607 are statistically indistinguishable, corroborating the recent result of Saffe et al. This could suggest that both stars accreted similar amounts of rocky material; indeed, our model for the chemical signature of rocky planet accretion indicates that HD 80606 could have accreted up to 2.5? of rocky material—about half that contained in the Solar System and primordial asteroid belt—relative to HD 80607 and still be consistent with the data. Since HD 80607 has no known giant planets that might have pushed rocky planet material via migration onto that star, we consider it more likely that HD 80606/07 experienced essentially no rocky planet accretion. This in turn suggests that the migration history of the HD 80606 giant planet must have been such that it ejected any close-in planetary material that might have otherwise been shepherded onto the star.
机译:我们使用Keck / HIRES光谱对行星宿主宽二元(PHWB)系统HD 80606 + HD 80607中的15种元素进行了详细的化学丰度分析。正如我们之前对PHWB HD 20782 + HD 20781的分析一样,我们假设这两个G5矮星一起形成,因此具有相同的原始丰度。在此二进制文件中,HD 80606在〜0.5 AU处拥有一个偏心()巨型行星,但HD 80607没有检测到行星。如果偏心轨道上的近距离巨型行星能够有效地将岩石行星材料散射到它们的宿主恒星中,那么HD 80606应该显示出已经吸收了岩石材料的证据,而HD 80607应该没有。在这里,我们表明HD 80606和HD 80607的丰度与元素冷凝温度的趋势在统计上是无法区分的,从而证实了Saffe等人的最新结果。这可能表明两个恒星都吸收了相似数量的岩石物质。确实,我们的岩石行星增生化学特征模型表明HD 80606可能增生了2.5?相对于HD 80607,岩石材料的含量(大约是太阳系和原始小行星带的一半)仍与数据一致。由于HD 80607没有已知的巨行星,可能通过迁移将岩石行星的物质推到该恒星上,因此我们认为HD 80606/07基本上没有岩石行星增生的可能性。这反过来表明,HD 80606巨型行星的迁移历史一定是这样的,它会喷射出任何可能被束缚到恒星上的近距离行星物质。

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