吸积中子星的热释放

M. Gusakov, A. Chugunov
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引用次数: 3

摘要

在静止状态下,从吸积中子星(NSs)观察到的热发射被认为是由加热恒星地壳的非平衡核反应提供能量的(深部地壳加热范式)。我们推导了一个简单的热效率的通用公式,假设一个行星有一个完全增生的地壳。我们进一步表明,在最近提出的吸积地壳的热力学一致性方法中,热量释放可以用唯一的一个参数来参数化-地壳内外界面的压力$P_{\rm oi}$(正如我们所认为的,这个压力不一定与中子滴压一致)。我们讨论了考虑壳层效应的核模型中$P_{\rm oi}$的可能值,并确定了净热释放及其在地壳中的分布作为$P_{\rm oi}$的函数。我们得出的结论是,与以前的作品相比,放热应减少几个因素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Heat release in accreting neutron stars
Observed thermal emission from accreting neutron stars (NSs) in a quiescent state is believed to be powered by nonequilibrium nuclear reactions that heat the stellar crust (deep crustal heating paradigm). We derive a simple universal formula for the heating efficiency, assuming that an NS has a fully accreted crust. We further show that, within the recently proposed thermodynamically consistent approach to the accreted crust, the heat release can be parametrized by the only one parameter -- the pressure $P_{\rm oi}$ at the outer-inner crust interface (as we argue, this pressure should not necessarily coincide with the neutron-drip pressure). We discuss possible values of $P_{\rm oi}$ for a selection of nuclear models that account for shell effects, and determine the net heat release and its distribution in the crust as a function of $P_{\rm oi}$. We conclude that the heat release should be reduced by a factor of few in comparison to previous works.
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