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SURFACE MODES ON BURSTING NEUTRON STARS AND X-RAY BURST OSCILLATIONS

机译:爆发中子星和X射线爆发振荡的表面模式

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摘要

Accreting neutron stars (NSs) often show coherent modulations during type I X-ray bursts, called burst oscillations. We consider whether a nonradial mode can serve as an explanation for burst oscillations from those NSs that are not magnetic. We find that a surface wave in the shallow burning layer changes to a crustal interface wave as the envelope cools, a new and previously uninvestigated phenomenon. The surface modulations decrease dramatically as the mode switches, explaining why burst oscillations often disappear before burst cooling ceases. When we include rotational modifications, we find mode frequencies and drifts consistent with those observed. The large NS spin ( ≈ 270-620 Hz) needed to make this match implies that accreting NSs are spinning at frequencies ≈ 4 Hz above the burst oscillation. Since the long-term stable asymptotic frequency is set by the crustal interface wave, the observed late-time frequency drifts are a probe of the composition and temperature of NS crusts. We compare our model with the observed drifts and persistent luminosities of X-ray burst sources and find that NSs with a higher average accretion rate show smaller drifts, as we predict. Furthermore, the drift sizes are consistent with crusts composed of iron-like nuclei, as expected for the ashes of the He-rich bursts that are exhibited by these objects.
机译:积聚的中子星(NSs)在I型X射线爆发期间通常表现出相干调制,称为爆发振荡。我们考虑非径向模式是否可以解释非磁性NS的突发振荡。我们发现,随着包壳的冷却,浅层燃烧层中的表面波变成了地壳界面波,这是一种新的,以前未曾研究过的现象。随着模式的切换,表面调制急剧降低,这解释了为什么爆裂振荡通常在爆裂冷却停止之前就消失了。当我们包括旋转修改时,我们发现模式频率和漂移与观察到的一致。进行此匹配所需的较大的NS自旋(≈270-620 Hz)表示,吸积的NS在高于猝发振荡≈4 Hz的频率处旋转。由于长期稳定的渐近频率是由地壳界面波设定的,因此观察到的后期频率漂移是NS壳成分和温度的一个探查。我们将模型与观察到的X射线猝发源的漂移和持续发光度进行比较,发现平均吸积率较高的NSs的漂移较小,正如我们预测的那样。此外,漂移大小与由铁状核组成的地壳一致,正如这些物体所表现出的富含He的爆发灰烬所预期的那样。

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