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Nuclear heating and melted layers in the inner crust of an accreting neutron star

机译:核加热和内部地壳融化的融化层   中子星

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摘要

A neutron star in a long-lived, low-mass binary can easily accrete enoughmatter to replace its entire crust. Previous authors noted that an accretedcrust, being formed from the burning of accreted hydrogen and helium, allows aseries of non-equilibrium reactions, at densities >6e11 g/cc, which release asubstantial amount of heat (1 MeV per accreted nucleon). Recent calculations bySchatz et al. showed that the crystalline lattice of an accreted crust is alsolikely to be quite impure. This paper discusses the thermal structure of such aneutron star and surveys how the crust reactions and impurities affect thecrust temperature. During accretion rapid enough to make the accreted hydrogenand helium burn stably (near the Eddington accretion rate; typical of thebrightest low-mass neutron star binaries), most of the heat released in thecrust is conducted into the core, where neutrino emission regulates thetemperature. As a result there is an inversion of the thermal gradient: thetemperature decreases with depth in the inner crust. The thermal structure inthe crust at these high accretion rates is insensitive to the temperature inthe hydrogen/helium burning shell. When the crust is very impure, thetemperature can reach approximately 8e8 K at densities > 6e11 g/cc. This peaktemperature depends mostly on the amount of heat released and the thermalconductivity and in particular is roughly independent of the core temperature.The high crust temperatures are sufficient to melt the crystalline lattice inthin layers where electron captures have substantially reduced the nuclearcharge.
机译:长寿命,低质量双星中的中子星很容易积聚足够的物质来代替其整个地壳。先前的作者指出,由积聚的氢和氦气燃烧形成的积垢壳,允许一系列密度> 6e11 g / cc的非平衡反应,释放出大量的热量(每个积聚的核子1 MeV)。 Schatz等人的最新计算。结果表明,积垢的地壳的晶格也很不纯净。本文讨论了这种中子星的热结构,并调查了地壳反应和杂质如何影响地壳温度。在吸积过程中足够快以使吸出的氢和氦稳定地燃烧(接近爱丁顿的吸积率;典型的最明亮的低质量中子星双星),地壳中释放的大部分热量传导到堆芯,中微子的发射调节温度。结果是热梯度发生了逆转:温度随着内壳的深度而降低。在这些高积聚速率下,地壳中的热结构对氢/氦燃烧壳中的温度不敏感。当地壳非常不纯时,密度> 6e11 g / cc时温度可以达到大约8e8K。这个峰值温度主要取决于释放的热量和导热率,特别是大致上与堆芯温度无关。高地壳温度足以融化薄层中的晶格,其中电子俘获已大大降低了核电荷。

著录项

  • 作者

    Brown, Edward F.;

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  • 年度 1999
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  • 原文格式 PDF
  • 正文语种 {"code":"en","name":"English","id":9}
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