论文标题

通过外壳界面模式探测中子星中的相变

Probing phase transition in neutron stars via the crust-core interfacial mode

论文作者

Zhu, Jiaxiang, Wang, Chuming, Xia, Chengjun, Zhou, Enping, Ma, Yiqiu

论文摘要

从二进制中子恒星(BNS)系统发出的引力波可以携带有关这些紧凑型恒星中密集物质相的信息。地壳核界面模式是中子恒星中的振荡模式,它主要取决于地壳核过渡区域中物质状态的方程。可以通过Inspiral-In-In BNS系统的潮汐场来共鸣,从而影响发射的重力波,因此可以使用来探测外壳核心过渡区域中状态方程。在这项工作中,我们详细研究了中子恒星内部的一阶相变,如何利用牛顿流体扰动理论在恒星结构的一般相对论背景解决方案上使用牛顿流体扰动理论。考虑了两种可能的相变类型:(1)相变发生在流体芯中,但在地壳核界面附近发生,从而导致密度不连续; (2)密集芯中的强相互作用相变(如常规杂化恒星案例中)。讨论了这些相变对界面模式属性的影响。特别是,以前的相变对M-R关系和绝热潮汐变形性有很小的影响,但可以显着影响界面模式频率,从而可以使用重力波探测。对于BNS系统,我们讨论了重力波形中这些相变的可能的观察性特征及其可检测性。我们的工作丰富了对地壳核心界面模式的物理特性的探索,并提供了一种有前途的方法来使用紧凑型星的地震学探测相变。

Gravitational waves emitted from the binary neutron star (BNS) systems can carry information about the dense matter phase in these compact stars. The crust-core interfacial mode is an oscillation mode in a neutron star and it depends mostly on the equation of the state of the matter in the crust-core transition region. This mode can be resonantly excited by the tidal field of an inspiraling-in BNS system, thereby affecting the emitted gravitational waves, and hence could be used to probe the equation of state in the crust-core transition region. In this work, we investigate in detail how the first-order phase transition inside the neutron star affects the properties of the crust-core interfacial mode, using a Newtonian fluid perturbation theory on a general relativistic background solution of the stellar structure. Two possible types of phase transitions are considered: (1) the phase transitions happen in the fluid core but near the crust-core interface, which results in density discontinuities; and (2) the strong interaction phase transitions in the dense core (as in the conventional hybrid star case). These phase transitions' impacts on interfacial mode properties are discussed. In particular, the former phase transition has a minor effect on the M-R relation and the adiabatic tidal deformability, but can significantly affect the interfacial mode frequency and thereby could be probed using gravitational waves. For the BNS systems, we discuss the possible observational signatures of these phase transitions in the gravitational waveforms and their detectability. Our work enriches the exploration of the physical properties of the crust-core interfacial mode and provides a promising method for probing the phase transition using the seismology of a compact star.

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