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首页> 外文期刊>The Astrophysical Journal. Supplement Series >A survey of the parameter space of the compressible liquid drop model as applied to the neutron star inner crust
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A survey of the parameter space of the compressible liquid drop model as applied to the neutron star inner crust

机译:可压缩液滴模型应用于中子星内壳的参数空间研究

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We present a systematic survey of the range of predictions of the neutron star inner crust composition, crust-core transition densities and pressures, and density range of the nuclear "pasta" phases at the bottom of the crust provided by the compressible liquid drop model in light of the current experimental and theoretical constraints on model parameters. Using a Skyrme-like model for nuclear matter, we construct baseline sequences of crust models by consistently varying the density dependence of the bulk symmetry energy at nuclear saturation density, L, under two conditions: (1) that the magnitude of the symmetry energy at saturation density J is held constant, and (2) J correlates with L under the constraint that the pure neutron matter (PNM) equation of state (EoS) satisfies the results of ab initio calculations at low densities. Such baseline crust models facilitate consistent exploration of the L dependence of crustal properties. The remaining surface energy and symmetric nuclear matter parameters are systematically varied around the baseline, and different functional forms of the PNM EoS at sub-saturation densities implemented, to estimate theoretical "error bars" for the baseline predictions. Inner crust composition and transition densities are shown to be most sensitive to the surface energy at very low proton fractions and to the behavior of the sub-saturation PNM EoS. Recent calculations of the energies of neutron drops suggest that the low-proton-fraction surface energy might be higher than predicted in Skyrme-like models, which our study suggests may result in a greatly reduced volume of pasta in the crust than conventionally predicted.
机译:我们对中子星内壳组成,壳核过渡密度和压力以及壳底可压缩液滴模型提供的底部“核”相的密度范围的预测范围进行了系统的调查。参照当前对模型参数的实验和理论约束。使用类似于Skyrme的核物质模型,我们通过在两个条件下持续改变核对称密度L下的体对称能量的密度依赖性来构造地壳模型的基线序列:(1)饱和密度J保持恒定,并且(2)在纯中子状态方程(EoS)满足低密度从头算结果的约束下,J与L相关。这样的基线地壳模型有利于对地壳性质的L依赖性的一致探索。剩余的表面能和对称核物质参数在基线附近系统地变化,并且在亚饱和密度下实施了不同功能形式的PNM EoS,以估计基线预测的理论“误差线”。内壳成分和过渡密度对质子分数非常低时的表面能以及亚饱和PNM EoS的行为最为敏感。最近对中子滴能量的计算表明,低质子分数的表面能可能比Skyrme型模型中的预测要高,我们的研究表明这可能导致地壳中的面食量比传统预测的大大减少。

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