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A REMARKABLE 3 HOUR THERMONUCLEAR BURST FROM 4U 1820― 30

机译:4U 1820〜30的3小时热爆发

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摘要

We present a detailed observational and theoretical study of a ~3 hr long X-ray burst (the " superburst") observed by the Rossi X-Ray Timing Explorer (RXTE) from the low-mass X-ray binary 4U 1820 ― 30. This is the longest X-ray burst ever observed from this source and perhaps one of the longest ever observed in great detail from any source. We show that the superburst is thermonuclear in origin. Its peak luminosity of ~3.4 x 10~(38) ergs s~(-1) is consistent with the helium Eddington limit for a neutron star at ~ 7 kpc as well as the peak luminosity of other, shorter, thermonuclear bursts from the same source; The superburst begins in the decaying tail of a more typical (≈20 s duration) thermonuclear burst. These shorter, more frequent bursts are well-known helium flashes from this source. The level of the accretion-driven flux as well as the observed energy release of upward of 1.5 x 10~(42) ergs indicate that helium could not be the energy source for the superburst. We outline the physics relevant to carbon production and burning on helium-accreting neutron stars and present calculations of the thermal evolution and stability of a carbon layer and show that this process is the most likely explanation for the superburst. Ignition at the temperatures in the deep carbon " ocean " requires more than 30 times the mass of carbon inferred from the observed burst energetics unless the He flash is able to trigger a deflagration from a much smaller mass of carbon. We show, however, that for large columns of accreted carbon fuel, a substantial fraction of the energy released in the carbon-burning layer is radiated away as neutrinos, and the heat that is conducted from the burning layer in large part flows inward, only to be released on timescales longer than the observed burst. Thus, the energy released during the event possibly exceeds that observed in X-rays by more than a factor of 10, making the scenario of burning a large mass of carbon at great depths consistent with the observed fluence without invoking any additional trigger. A strong constraint on this scenario is the recurrence time: to accrete an ignition column of 10~(13) g cm~(-2) takes ~13/(M/3 x 10~(17) g s~(-1)) yr. Spectral analysis during the superburst reveals the presence of a broad emission line between 5.8 and 6.4 keV and an edge at 8―9 keV, likely due to reflection of the burst flux from the inner accretion disk in 4U 1820―30. We believe that this is the first time such a signature has been unambiguously detected in the spectrum of an X-ray burst.
机译:我们提供了罗西X射线定时探测器(RXTE)从低质量X射线二进制4U 1820〜30观测到的约3小时长的X射线爆发(“超爆”)的详细观察和理论研究。这是有史以来从该源观察到的最长的X射线爆发,也许是有史以来从任何源头观察到的最详细的最长的X射线爆发之一。我们证明了这种超爆源是热核的。它的峰值光度约为3.4×10〜(38)ergs s〜(-1),与中子星在〜7 kpc时的爱丁顿氦极限以及与之相同的其他更短的热核爆发的峰值光度一致。资源;超级爆发始于更典型的(约20 s持续时间)热核爆发的衰变尾巴。这些更短,更频繁的爆发是此来源的著名氦闪光。吸积驱动的通量水平以及观察到的能量释放超过1.5 x 10〜(42)ergs,表明氦气不能成为爆炸的能量来源。我们概述了与产生碳和在吸收氦的中子星上燃烧有关的物理学,并给出了碳层热演化和稳定性的计算,并表明该过程是最可能解释超爆的原因。在深碳“海洋”中的温度下点火需要的质量是从观测到的爆发能学推断出的碳质量的30倍以上,除非He闪光灯能够触发小得多的碳质量引起的爆燃。但是,我们表明,对于大列的积碳燃料,碳燃烧层释放的大部分能量都作为中微子散发出去,并且从燃烧层传导的热量大部分向内流动,仅以比观察到的爆发更长的时间尺度释放。因此,事件期间释放的能量可能会比在X射线中观察到的能量大10倍以上,从而使在较大深度燃烧大量碳的场景与所观察到的注量一致,而无需调用任何其他触发器。在这种情况下,重现时间是一个很强的约束条件:要增加10〜(13)g cm〜(-2)的点火柱,大约需要花费13 /(M / 3 x 10〜(17)gs〜(-1))。年。在超爆过程中的光谱分析表明,存在一个在5.8和6.4 keV之间的宽发射线和一个在8-9 keV处的边缘,这可能是由于4U 1820-30中来自内部吸积盘的爆裂通量的反射所致。我们相信,这是第一次在X射线猝发光谱中明确检测到这种签名。

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