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Neutron star properties and the equation of state for the core

机译:中子星特性和核的状态方程

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Context. Few unified equations of state for neutron star matter, in which core and crust are described using the same nuclear model, are available. However the use of non-unified equations of state with simplified matching between the crust and core has been shown to introduce uncertainties in the radius determination, which can be larger than the expected precision of the next generation of X-ray satellites. Aims. We aim to eliminate the dependence of the radius and mass of neutron stars on the detailed model for the crust and on the crust-core matching procedure. Methods. We solved the approximate equations of the hydrostatic equilibrium for the crust of neutron stars and obtained a precise formula for the radius that only depends on the core mass and radius, the baryon chemical potential at the core-crust interface, and at the crust surface. For a fully accreted crust one needs, additionally, the value of the total deep crustal heating per one accreted nucleon. Results. For typical neutron star masses, the approximate approach allows us to determine the neutron star radius with an error ~ 0.1% ( ~ 10 m, equivalent to a 1% inaccuracy in the crust thickness). The formalism applies to neutron stars with a catalyzed or a fully accreted crust. The difference in the neutron star radius between the two models is proportional to the total energy release due to deep crustal heating. Conclusions. For a given model of dense matter describing the neutron star core, the radius of a neutron star can be accurately determined independent of the crust model with a precision much better than the ~ 5% precision expected from the next generation of X-ray satellites. This allows us to circumvent the problem of the radius uncertainty that may arise when non-unified equations of state for the crust and core are used.
机译:上下文。几乎没有统一的中子星物质状态方程,其中使用相同的核模型描述了核和壳。但是,已经证明使用地壳与岩心之间具有简化匹配的非统一状态方程会在半径确定中引入不确定性,该不确定性可能大于下一代X射线卫星的预期精度。目的我们旨在消除中子星的半径和质量对地壳的详细模型以及地壳-铁心匹配程序的依赖性。方法。我们求解了中子星地壳的静水力平衡近似方程,并获得了仅取决于堆芯质量和半径,堆芯-地壳界面以及地壳表面的重子化学势的半径的精确公式。对于完全积聚的地壳,还需要每一个积聚的核子的总深地壳加热值。结果。对于典型的中子星质量,近似方法使我们能够确定中子星半径,误差为〜0.1%(〜10 m,相当于地壳厚度的1%不准确度)。形式论适用于带有催化或完全积聚的地壳的中子星。两种模型之间中子星半径的差异与由于深地壳加热而释放的总能量成正比。结论。对于描述中子星核的致密模型的给定模型,可以精确地确定中子星的半径,而与地壳模型无关,其精度要比下一代X射线卫星预期的〜5%精度好得多。这使我们能够规避当使用地壳和岩心的非统一状态方程时可能出现的半径不确定性问题。

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