论文标题

紧凑型二进制的延迟合并后建模:相对论,R过程加热和运输效应的处理

Late-time post-merger modeling of a compact binary: effects of relativity, r-process heating, and treatment of transport effects

论文作者

Haddadi, Milad, Duez, Matthew D., Foucart, Francois, Ramirez, Teresita, Fernandez, Rodrigo, Knight, Alexander L., Jesse, Jerred, Hebert, Francois, Kidder, Lawrence E., Pfeiffer, Harald P., Scheel, Mark A.

论文摘要

合并后的前十秒钟,可以通过黑洞 - 核酸磁盘残留物中的流出来产生与紧凑型二进制合并引力的可检测的电磁对应物。具有有效粘度的二维轴对称模拟仍然是一种有效且有益的方法,可以建模这种延迟时间后连续性后的演化。除了轴对称性的固有近似值和通过粘度建模湍流角动量传输外,先前的模拟通常会使其他简化与状态方程和湍流效应方程的处理有关。 在本文中,我们测试了这些建模选择的效果。通过以相同的粘度发展,以前在牛顿粘性流体动力学中进化的确切合并后初始构型,我们发现牛顿的处理提供了对磁盘弹出质量的良好估计,但低估了流速速度。我们发现,重核的包含会导致射流质量显着增加。 R-Process效应的大致包含的效果相对较小,除了其对组成的设计效应。成分和熵的扩散,建模湍流传输效应,具有减少弹射质量的总体效果,并以较低的平均水平和更紧密的分布为速度。同样,我们发现即使在10,000 \ km以上的距离处,流出的加速度显着,因此热风速仅渐近性超出了这一半径,并且比以前报道的要高的值更高。

Detectable electromagnetic counterparts to gravitational waves from compact binary mergers can be produced by outflows from the black hole-accretion disk remnant during the first ten seconds after the merger. Two-dimensional axisymmetric simulations with effective viscosity remain an efficient and informative way to model this late-time post-merger evolution. In addition to the inherent approximations of axisymmetry and modeling turbulent angular momentum transport by a viscosity, previous simulations often make other simplifications related to the treatment of the equation of state and turbulent transport effects. In this paper, we test the effect of these modeling choices. By evolving with the same viscosity the exact post-merger initial configuration previously evolved in Newtonian viscous hydrodynamics, we find that the Newtonian treatment provides a good estimate of the disk ejecta mass but underestimates the outflow velocity. We find that the inclusion of heavy nuclei causes a notable increase in ejecta mass. An approximate inclusion of r-process effects has a comparatively smaller effect, except for its designed effect on the composition. Diffusion of composition and entropy, modeling turbulent transport effects, has the overall effect of reducing ejecta mass and giving it a speed with lower average and more tightly-peaked distribution. Also, we find significant acceleration of outflow even at distances beyond 10,000\,km, so that thermal wind velocities only asymptote beyond this radius and at somewhat higher values than previously reported.

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