论文标题
重新审视强磁场和意大利面相
Strong magnetic fields and pasta phases revisited
论文作者
论文摘要
在这项工作中,我们计算出在强磁场存在下中子恒星内皮的结构和组成,例如可以在磁场中找到。为了确定地壳不均匀性的几何形状和特征,我们考虑了可压缩的液滴模型,其中表面和库仑术语包括在变化方程中,我们将结果与基于更多近似处理的先前计算进行了比较。对于状态方程(EOS),我们考虑了两个非线性相对论平均模型,具有对称能的不同斜率,并且我们表明,由于磁场,恒星核心内部不均匀区域的扩展很大程度上取决于地壳EOS中鉴别能的行为。最后,我们认为在先前计算中观察到的扩展的旋转不稳定性可能与磁体外芯中的幅度密度波动的存在有关,而不是与较厚的固体外壳有关。可压缩的液态滴模型形式主义虽然与先前的计算总体一致,但会导致对亚稳态溶液的系统抑制,从而可以更精确地估计地壳核心的过渡密度和压力,从而更好地估计地壳半径。
In this work, we compute the structure and composition of the inner crust of a neutron star in the presence of a strong magnetic field, such as it can be found in magnetars. To determine the geometry and characteristics of the crust inhomogeneities, we consider the compressible liquid drop model, where surface and Coulomb terms are included in the variational equations, and we compare our results with previous calculations based on more approximate treatments. For the equation of state (EoS), we consider two non-linear relativistic mean-field models with different slopes of the symmetry energy, and we show that the extension of the inhomogeneous region inside the star core due to the magnetic field strongly depends on the behavior of the symmetry energy in the crustal EoS. Finally, we argue that the extended spinodal instability observed in previous calculations can be related to the presence of small amplitude density fluctuations in the magnetar outer core, rather than to a thicker solid crust. The compressible liquid drop model formalism, while in overall agreement with the previous calculations, leads to a systematic suppression of the metastable solutions, thus allowing a more precise estimation of the crust-core transition density and pressure, and therefore a better estimation of the crustal radius.