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arXiv 2408.04411astro-ph.EPastro-ph.GAastro-ph.SRgr-qc
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分级三体系统动力学中的高阶效应。II. 二阶与三十二极阶效应

Higher-order effects in the dynamics of hierarchical triple systems. II. Second-order and dotriacontapole-order effects

Landen Conway, Clifford M. Will

AI总结:

本文用双时间尺度方法推导分级三体系统至四极摄动二阶和 ε^6 的长期演化方程,揭示三十二极贡献及二阶下半长轴不再恒定但总能量守恒。

摘要:

我们分析了牛顿引力下分级三体系统的长期演化,计算至四极矩摄动参数的二阶,以及 ε=a/A 的六阶,其中 ε 是内轨道与外轨道半长轴之比。我们将应用数学中的“双时间尺度”方法用于内、外轨道的拉格朗日行星方程;在该方法中,每个密切轨道要素都被分解为在长摄动时间尺度上演化的轨道平均部分,以及在轨道时间尺度上振荡的“无平均”部分。对两个轨道时间尺度的平均采用众所周知的长期近似来完成。我们还纳入了时间与轨道相位之间关系的摄动修正。除要求四极矩参数和 ε 都很小之外,我们对质量、相对轨道倾角或偏心率均不作任何限制。结果得到一整套关于内、外轨道平均要素的长时间尺度演化方程。在摄动理论一阶,我们在 ε^6 阶显式得到三十二极贡献。在摄动理论二阶,即四极矩摄动振幅的二次项,我们发现了按 ε^{9/2}(在早期工作中已发现)、ε^5、ε^{11/2} 和 ε^6 缩放的贡献。在一阶摄动和三十二极阶,两个平均半长轴在时间上保持恒定(并且我们证明这一结论对任意多极阶均成立);但在二阶摄动中,从 O(ε^5) 开始,它们不再恒定。尽管如此,我们验证了系统的总平均能量是守恒的,并论证这一行为与关于半长轴长期演化的经典定理并不矛盾。

英文摘要:

We analyze the long-term evolution of hierarchical triple systems in Newtonian gravity to second order in the quadrupolar perturbation parameter, and to sixth order in $ε= a/A$, the ratio of the semimajor axes of the inner and outer orbits. We apply the ``two-timescale'' method from applied mathematics to the Lagrange Planetary Equations for the inner and outer orbits, in which each osculating orbit element is split into an orbit averaged part that evolves on the long perturbative timescale, and an ``average-free'' part that is oscillatory in the orbital timescales. Averages over the two orbital timescales are performed using the well-known secular approximation. We also incorporate perturbative corrections to the relation between time and the orbital phases. We place no restrictions on the masses, on the relative orbit inclinations or on the eccentricities, beyond the requirement that the quadrupolar parameter and $ε$ both be small. The result is a complete set of long-timescale evolution equations for the averaged elements of the inner and outer orbits. At first order in perturbation theory, we obtain the dotriacontapole contributions explicitly at order $ε^6$. At second order in perturbation theory, i.e. quadratic in the quadrupole perturbation amplitude, we find contributions that scale as $ε^{9/2}$ (found in earlier work), $ε^{5}$, $ε^{11/2}$, and $ε^{6}$. At first perturbative order and dotriacontapole order, the two averaged semimajor axes are constant in time (and we prove that this holds to arbitrary multipole orders); but at second perturbative order, beginning at $O( ε^{5})$, they are no longer constant. Nevertheless we verify that the total averaged energy of the system is conserved, and we argue that this behavior is not incompatible with classical theorems on secular evolution of the semimajor axes.

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