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arXiv 1906.06705gr-qcastro-ph.EPphysics.space-ph
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后牛顿重力试验中的平均距平和平均经度

On the mean anomaly and the mean longitude in tests of post-Newtonian gravity

Lorenzo Iorio

摘要:

平均距平$\mathcal{M}(t)$与历元$η$的平均距平之间的区别,以及平均经度$l(t)$与历元$ε$的平均经度之间的区别,在后开普勒重力检验中可能使用这些轨道要素的背景下得到澄清,包括牛顿和后牛顿。特别地,对于任意的测试粒子轨道构型和初级粒子自旋轴$\boldsymbol{\hat{S}}$的一般取向,计算了后牛顿Schwarzschild和Lense-Thirring场对$\mathcal{M}(t),\,η,\,l(t),\,ε$的扰动,以及大气阻力和中心体扁率$J_2$引起的经典加速度.它们为我们提供了可以有效利用的进一步的可观察性,例如,在更好地描述天体物理学双星系统和更准确的太阳系主要天体周围的卫星测试方面。一些错误的和误导性的索赔Ciufolini和帕夫利斯出现在文献中驳斥。特别是,它表明,有没有净扰动的透镜-Thirring加速度上的半长轴$a$和平均运动$n_\mathrm{b}$。此外,由于某些干扰性的非重力加速度(如大气阻力),$\mathcal{M}(t)$和$l(t)$上的二次签名可以有效地从后牛顿线性趋势中解脱出来,只要假设数据分析的时间间隔足够长。提出了利用现有的LAGEOS和LAGEOS II卫星进行广义相对论检验时,可能使用$η$和升交点$Ω$的交点。

英文摘要:

The distinction between the mean anomaly $\mathcal{M}(t)$ and the mean anomaly at epoch $η$, and the mean longitude $l(t)$ and the mean longitude at epoch $ε$ is clarified in the context of a possible use of such orbital elements in post-Keplerian tests of gravity, both Newtonian and post-Newtonian. In particular, the perturbations induced on $\mathcal{M}(t),\,η,\,l(t),\,ε$ by the post-Newtonian Schwarzschild and Lense-Thirring fields, and the classical accelerations due to the atmospheric drag and the oblateness $J_2$ of the central body are calculated for an arbitrary orbital configuration of the test particle and a general orientation of the primary's spin axis $\boldsymbol{\hat{S}}$. They provide us with further observables which could be fruitfully used, e.g., in better characterizing astrophysical binary systems and in more accurate satellite-based tests around major bodies of the Solar System. Some erroneous and misleading claims by Ciufolini and Pavlis appeared in the literature are confuted. In particular, it is shown that there are no net perturbations of the Lense-Thirring acceleration on either the semimajor axis $a$ and the mean motion $n_\mathrm{b}$. Furthermore, the quadratic signatures on $\mathcal{M}(t)$ and $l(t)$ due to certain disturbing non-gravitational accelerations like the atmospheric drag can be effectively disentangled from the post-Newtonian linear trends of interest provided that a sufficiently extended temporal interval for the data analysis is assumed. A possible use of $η$ along with the longitudes of the ascending node $Ω$ in tests of general relativity with the existing LAGEOS and LAGEOS II satellites is suggested.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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