{"title":"Post-Keplerian perturbations of the hyperbolic motion in the field of a massive, rotating object","authors":"Lorenzo Iorio","doi":"arxiv-2409.12063","DOIUrl":null,"url":null,"abstract":"The perturbations of the hyperbolic motion of a test particle due to the\ngeneral relativistic gravitoelectromagnetic Schwarzschild and Lense-Thirring\ncomponents of the gravitational field of a massive, rotating body are\nanalytically worked out to the first post-Newtonian level. To the Newtonian\norder, the impact of the quadrupole mass moment of the source is calculated as\nwell. The resulting analytical expressions are valid for a generic orientation\nin space of both the orbital plane of the probe and the spin axis of the\nprimary, and for arbitrary values of the eccentricity. They are applied first\nto 'Oumuamua, an interstellar asteroid which recently visited our solar system\nalong an unbound heliocentric orbit. While its gravitoelectric shifts occurred\nclose to the Sun's flyby are less than some tens of milliarcseconds, those due\nto the solar oblateness and angular momentum are of the order of\nmicroarcseconds throughout the whole trajectory. Comparable values occur for\nthe post-Newtonian shifts of the Near Earth Asteroid Rendezvous (NEAR)\nspacecraft during its flyby of the Earth, while those due to the oblateness of\nthe latter are nominally several orders of magnitude larger. The current\n(formal) uncertainty in the quadrupole mass moment of the geopotential would\nbring the mismodeling of such classical effects below the nominal value of the\npredicted relativistic disturbances. The hyperbolic excess velocity is not\nchanged by any of the post--Keplerian accelerations considered. The\ncalculational approach developed can be straightforwardly extended to any\nalternative models of gravity as well.","PeriodicalId":501423,"journal":{"name":"arXiv - PHYS - Space Physics","volume":"157 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-09-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"arXiv - PHYS - Space Physics","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/arxiv-2409.12063","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
The perturbations of the hyperbolic motion of a test particle due to the
general relativistic gravitoelectromagnetic Schwarzschild and Lense-Thirring
components of the gravitational field of a massive, rotating body are
analytically worked out to the first post-Newtonian level. To the Newtonian
order, the impact of the quadrupole mass moment of the source is calculated as
well. The resulting analytical expressions are valid for a generic orientation
in space of both the orbital plane of the probe and the spin axis of the
primary, and for arbitrary values of the eccentricity. They are applied first
to 'Oumuamua, an interstellar asteroid which recently visited our solar system
along an unbound heliocentric orbit. While its gravitoelectric shifts occurred
close to the Sun's flyby are less than some tens of milliarcseconds, those due
to the solar oblateness and angular momentum are of the order of
microarcseconds throughout the whole trajectory. Comparable values occur for
the post-Newtonian shifts of the Near Earth Asteroid Rendezvous (NEAR)
spacecraft during its flyby of the Earth, while those due to the oblateness of
the latter are nominally several orders of magnitude larger. The current
(formal) uncertainty in the quadrupole mass moment of the geopotential would
bring the mismodeling of such classical effects below the nominal value of the
predicted relativistic disturbances. The hyperbolic excess velocity is not
changed by any of the post--Keplerian accelerations considered. The
calculational approach developed can be straightforwardly extended to any
alternative models of gravity as well.