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Crustal Emission and the Quiescent Spectrum of the Neutron Star in KS 1731–260

机译:KS 1731–260中的地壳发射和中子星的静态光谱

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The type I X-ray-bursting low-mass X-ray binary KS 1731-260 was recently detected for the first time in quiescence by Wijnands et al. following a τob ≈ 13 yr outburst, which ended in 2001 February. We show that the emission area radius for a H atmosphere spectrum (possibly with a hard power-law component that dominates the emission above 3.5 keV) is consistent with that observed from other quiescent neutron star transients, R∞ = 23 km and examine possible IR counterparts for KS 1731-260. Unlike all other known transient neutron stars, the duration of this recent (and the only observed) outburst is as long as the thermal diffusion time of the crust. The large amount of heat deposited by reactions in the crust will have heated the crust to temperatures much higher than the equilibrium core temperature. As a result, the thermal luminosity currently observed from the neutron star is dominated not by the core but by the crust. This scenario implies that the mean outburst recurrence timescale found by Wijnands et al. (~200 yr) is a lower limit. Moreover, because the thermal emission is dominated by the hot crust, the level and the time evolution of quiescent luminosity is determined mostly by the amount of heat deposited in the crust during the most recent outburst (for which reasonable constraints on the mass accretion rate exist) and is only weakly sensitive to the core temperature. Using estimates of the outburst mass accretion rate, our calculations of the quiescent flux immediately following the end of the outburst agree with the observed quiescent flux to within a factor of a few. In this paper, we present simulations of the evolution of the quiescent light curve for different scenarios of the crust microphysics and demonstrate that monitoring observations (with currently flying instruments) spanning from 1 to 30 yr can measure the crust cooling timescale and the total amount of heat stored in the crust. These quantities have not been directly measured for any neutron star. This makes KS 1731-260 a unique laboratory for studying the thermal properties of the crust by monitoring the luminosity over the next few years to decades.
机译:Wijnands等人最近首次静态地检测到I型X射线爆裂低质量X射线二进制KS 1731-260。在τob≈13年爆发后,该爆发于2001年2月结束。我们表明,H大气光谱的发射面积半径(可能具有高于3.5 keV的主要功率定律的硬幂定律分量)与从其他静态中子星瞬变观测到的半径一致,R∞= 23 km,并检查了可能的IR适用于KS 1731-260。与所有其他已知的瞬变中子星不同,最近(也是唯一观察到的)爆发的持续时间与地壳的热扩散时间一样长。地壳中反应产生的大量热量会将地壳加热到比平衡核心温度高得多的温度。结果,目前从中子星观测到的热光度不是由核而是由壳构成。这种情况暗示了Wijnands等人发现的平均爆发复发时间尺度。 (〜200岁)是下限。此外,由于热量的释放主要由地壳决定,因此静态发光度的水平和时间演变主要由最近爆发期间地壳中沉积的热量决定(对此存在合理的质量吸收率约束) ),并且仅对核心温度敏感。使用对爆发质量积累率的估计,我们在爆发结束后立即计算出的静态通量与观测到的静态通量相差不大。在本文中,我们对地壳微观物理的不同情况下的静态光曲线的演化进行了仿真,并证明了监视观测(使用当前飞行的仪器)的时间跨度为1至30年,可以测量地壳冷却的时间尺度和总的冷却时间。热量储存在地壳中。这些量尚未对任何中子星直接测量。这使得KS 1731-260成为通过监视未来几年到几十年的光度来研究地壳热学性质的独特实验室。

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