论文标题

从振幅到重力辐射,具有立方相互作用和潮汐效应

From amplitudes to gravitational radiation with cubic interactions and tidal effects

论文作者

Huber, Manuel Accettulli, Brandhuber, Andreas, De Angelis, Stefano, Travaglini, Gabriele

论文摘要

我们研究了立方体和潮汐相互作用对两个非旋转对象合并的灵感阶段中发出的引力波的影响。有两个独立的平价 - 甚至三次的互动术语,我们认为这是$ i_1 = {r^{αβ}} _ {μν} {r^{μν}} _ {ρσ}} r^α\,_μ\,^β\,_νr^μ\,_ρ\,^ν\,_σr^ρ\,__α\,^σ\,_β$。后者具有消失的纯重力振幅,但修饰了混合标量/重力振幅,这对于我们的研究至关重要。在有效的现场理论设置中,我们根据$ i_1 $,$ g_3 $和潮汐相互作用来计算对四极力矩的修改,从中,我们从中获得了在过程中散发出的引力波的力量,以在扰动中进行一阶和后命中阶段的领先顺序。 $ i_1 $预测是新颖的,我们发现$ g_3 $的结果与潮汐扰动引起的已知四极矫正有关,尽管$ g_3 $耦合的物理起源与潜在的潮汐相互作用的有限尺寸效果无关。我们通过重新计算此类潮汐校正并提出明确的字段重新定义来证明这一点。在Newtonian后扩展中,我们的结果按领先顺序完成,对于$ G_3 $和TIDAL ICTORTONIONS的重力波通量为5pn,而6pn则为$ i_1 $。最后,我们计算对波形的相应修改。

We study the effect of cubic and tidal interactions on the spectrum of gravitational waves emitted in the inspiral phase of the merger of two non-spinning objects. There are two independent parity-even cubic interaction terms, which we take to be $I_1 = {R^{αβ}}_{μν} {R^{μν}}_{ρσ} {R^{ρσ}}_{αβ}$ and $G_3 = I_1-2 R^α\,_μ\,^β\,_ν R^μ\,_ρ\,^ν\,_σ R^ρ\,_α\,^σ\,_β$. The latter has vanishing pure graviton amplitudes but modifies mixed scalar/graviton amplitudes which are crucial for our study. Working in an effective field theory set-up, we compute the modifications to the quadrupole moment due to $I_1$, $G_3$ and tidal interactions, from which we obtain the power of gravitational waves radiated in the process to first order in the perturbations and leading order in the post-Minkowskian expansion. The $I_1$ predictions are novel, and we find that our results for $G_3$ are related to the known quadrupole corrections arising from tidal perturbations, although the physical origin of the $G_3$ coupling is unrelated to the finite-size effects underlying tidal interactions. We show this by recomputing such tidal corrections and by presenting an explicit field redefinition. In the post-Newtonian expansion our results are complete at leading order, which for the gravitational-wave flux is 5PN for $G_3$ and tidal interactions, and 6PN for $I_1$. Finally, we compute the corresponding modifications to the waveforms.

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