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首页> 外文期刊>The Astrophysical journal >Nuclear Heating and Melted Layers in the Inner Crust of an Accreting Neutron Star
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Nuclear Heating and Melted Layers in the Inner Crust of an Accreting Neutron Star

机译:积淀中子星内壳的核加热和融化层

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A neutron star in a long-lived, low-mass binary can easily accrete enough matter to replace its entire crust. Previous authors noted that an accreted crust, being formed from the burning of accreted hydrogen and helium, allows a series of nonequilibrium reactions, at densities 6 × 1011 g cm-3, which release a substantial amount of heat (~1 MeV per accreted nucleon). Recent calculations by Schatz et al. showed that the crystalline lattice of an accreted crust is also likely to be quite impure. This paper discusses the thermal structure of such a neutron star and surveys how the crust reactions and impurities affect the crust temperature. During accretion rapid enough to make the accreted hydrogen and helium burn stably ( ~ 10-8 M☉ yr-1; typical of the brightest low-mass neutron star binaries), most of the heat released in the crust is conducted into the core, where neutrino emission regulates the temperature. As a result there is an inversion of the thermal gradient: the temperature decreases with depth in the inner crust. The thermal structure in the crust at these high accretion rates is insensitive to the temperature in the hydrogen/helium burning shell. When the crust is very impure, the temperature can reach ≈8 × 108 K at densities 6 × 1011 g cm-3. This peak temperature depends mostly on the amount of heat released and the thermal conductivity and in particular is roughly independent of the core temperature. The high crust temperatures are sufficient to melt the crystalline lattice in thin layers where electron captures have substantially reduced the nuclear charge.
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取代其整个地壳。先前的作者指出,由积聚的氢气和氦气燃烧形成的积垢壳,允许一系列密度为6×1011 g cm-3的非平衡反应,释放出大量的热量(每个积聚的核子约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,足以使吸出的氢和氦稳定地燃烧(〜10-8M☉yr-1;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岩心中,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,密度为6×1011 g cm-3时温度可以达到≈8×108K。该峰值温度主要取决于所释放的热量和热导率,特别是大致上与堆芯温度无关。较高的地壳温度足以熔化薄层中的晶格,在薄层中,电子俘获已大大减少了核电荷。

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