从地壳破裂和引力波看中子星的极限自转速率

J. A. Morales and C. J. Horowitz
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引用次数: 0

摘要

观测到的中子星旋转速度不会超过其分裂速率的一半。这种极限旋转频率可能与它们的地壳强度有关。当恒星从吸积中旋转时,离心力会对地壳施加压力。我们对旋转的中子星进行了有限元模拟,发现地壳以大约一半的旋转速率破裂。由于微观物理学的不确定性,我们还没有确定这次失败后的地壳结构。相反,我们认为地壳可能以不对称的方式失效,并可能产生具有显著椭圆性的构型(惯性矩的分数差)。如果椭圆度很大,旋转的恒星会辐射引力波,这可能会限制进一步的自旋向上。这些恒星可能是LIGO/VIRGO和下一代引力波探测器的有希望的来源。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Limiting Rotation Rate of Neutron Stars from Crust Breaking and Gravitational Waves
Neutron stars are not observed to spin faster than about half their breakup rate. This limiting rotational frequency may be related to the strength of their crusts. As a star spins up from accretion, centrifugal forces stress the crust. We perform finite-element simulations of rotating neutron stars and find that the crust fails at rotation rates about half the breakup rate. Given uncertainties in microphysics, we have not determined the crust configuration after this failure. Instead, we argue that the crust may fail in an asymmetric way and could produce a configuration with a significant ellipticity (fractional difference in moments of inertia). If the ellipticity is large, a rotating star will radiate gravitational waves that may limit further spin-up. These stars may be promising sources for LIGO/VIRGO and next-generation gravitational-wave detectors.
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