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The thermal and compositional structure of the crust of an accreting neutron star.

机译:吸积中子星壳的热和组成结构。

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摘要

This thesis discusses the atmospheres, oceans, and crusts of accreting neutron stars. On accreting X-ray pulsars, the magnetic field focuses the accretion flow onto a small fraction of the stellar area and produces rapid local accretion rates in excess of the Eddington limit. The strong magnetic field then confines the accreted matter to depths where the lateral, pressure greatly exceeds B2/8π. The currents needed to confine the mountain are large enough to modify, by order unity, the magnetic field strength at the polar cap. Rapid compression at local accretion rates exceeding ten times the Eddington rate heats the atmosphere/ocean to temperatures of order 109 K at relatively low densities; for stars accreting pure helium, this causes unstable ignition of the ashes (mostly carbon) resulting from stable helium burning. This unstable carbon ignition can recur on timescales shorter than a day.; The ashes of hydrogen/helium burning eventually replace the original crust of a neutron star in a long-lived, low-mass x-ray binary. This replaced crust is of much lower thermal and electrical conductivity and contains layers of non-equilibrium reactions, which heat the deep crust and core. The thermal structure of the crust depends most sensitively on the composition of the crust at densities near neutron drip and is particularly insensitive (at near-Eddington accretion rates, appropriate for the brightest low-mass binaries) to the temperatures in the atmosphere. The deep crustal heating and low electrical conductivity drastically shorten the timescale for the diffusion of magnetic flux, and may be an important influence in the evolution of the magnetic field.; A signature of deep crustal heating is the quiescent emission from the slowly accreting neutron star transients. The heat released in the crust by the non-equilibrium reactions is thermally radiated from the neutron star surface during quiescence. The predicted quiescent luminosity has the correct magnitude to explain observations. Since the quiescent luminosity sets an upper bound to the core temperature, observations of neutron star transients also constrain the amount of heating by, e.g., viscous dissipation of a steady state r-mode.
机译:本文讨论了积聚中子星的大气,海洋和地壳。在积聚X射线脉冲星时,磁场会将积聚流聚焦到恒星区的一小部分,并产生超过爱丁顿极限的快速局部积聚率。然后,强磁场将堆积的物质限制在横向压力大大超过 B 2 /8π的深度。限制山峰所需的电流足够大,可以按阶次统一来修改极帽处的磁场强度。以超过埃丁顿速率的十倍的局部吸积速率进行快速压缩,以相对较低的密度将大气/海洋加热到10 9 K的温度。对于吸收纯氦气的恒星,这会由于稳定的氦气燃烧而导致灰烬(主要是碳)的不稳定着火。这种不稳定的碳着火可能会在不到一天的时间内发生。氢/氦燃烧的灰烬最终取代了长寿命,低质量的X射线双星中的中子星原本的外壳。更换后的地壳的导热性和导电性要低得多,并且包含不平衡反应层,这些反应会加热深部地壳和岩心。地壳的热结构最敏感地取决于中子滴落附近密度下的地壳成分,并且对大气温度特别不敏感(在接近爱丁顿的吸积率下,适合最明亮的低质量二元二进制数)。地壳深部加热和低电导率极大地缩短了磁通量扩散的时间尺度,并且可能是磁场演化的重要影响。地壳深部加热的特征是缓慢吸收的中子星瞬变产生的静态辐射。非平衡反应在地壳中释放的热量在静止过程中从中子星表面辐射出去。预测的静态光度具有正确的大小可以解释观察结果。由于静态发光度设定了核心温度的上限,因此对中子星瞬变的观察还通过例如稳态r-模式的粘性耗散来限制发热量。

著录项

  • 作者

    Brown, Edward Francis.;

  • 作者单位

    University of California, Berkeley.;

  • 授予单位 University of California, Berkeley.;
  • 学科 Physics Astronomy and Astrophysics.
  • 学位 Ph.D.
  • 年度 1999
  • 页码 123 p.
  • 总页数 123
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 天文学;
  • 关键词

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