考虑到潮汐变形的行星重力势能数学模型

А. V. Shatina, A. S. Borets
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摘要

研究目的本文研究了一颗在大质量吸引中心(恒星)引力场中运动的粘弹性行星、一颗卫星和一颗或多颗相对于吸引中心在开普勒椭圆轨道上运动的其他行星的引力势能。粘弹性行星以外的天体由物质点建模。在粘弹性理论的线性模型框架内,已经解决了寻找弹性位移矢量的问题。传统上,使用固体模型来确定地球重力场,而潮汐变形则以对位势模型系数进行微小修正的形式加以考虑。在这项工作中,粘弹性球模型被用来考虑潮汐效应。该研究课题与地球人造卫星运动的高精度预报、地球重力场的高精度测量有关。在这项研究中,V.G. Vilke 开发的渐近和分析方法被用于包含高刚度粘弹性元素的机械系统,以及经典力学和数学分析方法。图表使用 Octave 数学软件包绘制。通过计算球形区域的三重积分,解决了弹性理论的准静态问题,从而获得了可变形行星的重力势能公式。此外,考虑到月球、太阳和金星在外部点的固态潮汐效应,还计算了地球的重力势能。绘制的图表显示了地球引力势与时间的关系。本文建立的理论和数值结果表明,对地球引力势能的主要贡献来自月球和太阳。太阳系中其他行星的影响很小。考虑到潮汐效应,地球外围点的引力势能值既取决于该点在运动坐标系中的位置,也取决于天体的相对位置。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A mathematical model of the gravitational potential of the planet taking into account tidal deformations
Objectives. This paper investigates the gravitational potential of a viscoelastic planet moving in the gravitational field of a massive attracting center (star), a satellite and one or more other planets moving in Keplerian elliptical orbits relative to the attracting center. Celestial bodies other than a viscoelastic planet are modeled by material points. Within the framework of the linear model of the theory of viscoelasticity, the problem of finding the vector of elastic displacement has been resolved. Traditionally, a solid body model is used to determine the Earth’s gravitational field, while tidal deformations are taken into account in the form of small corrections to the coefficients of the geopotential model. In this work, the viscoelastic ball model is used to take into account tidal effects. The relevance of the research topic is associated with high-precision forecasting of the movement of artificial satellites of the Earth, high-precision measurement of the Earth’s gravitational field.Methods. In this study the asymptotic and analytical methods developed by V.G. Vilke are used for mechanical systems containing viscoelastic elements of high rigidity, as well as methods of classical mechanics, mathematical analysis. The graphs were plotted using the Octave mathematical package.Results. After resolving the quasi-static problem of elasticity theory by calculating triple integrals over a spherical area, a formula for the gravitational potential of a deformable planet was obtained. In addition, the gravitational potential of the Earth was also calculated taking into account solid-state tidal effects from the Moon, Sun, and Venus at an external point. Graphs were constructed to show the dependence of the Earth’s gravitational potential on time.Conclusions. The theoretical and numerical results established herein show that the main contribution to the gravitational potential of the Earth is made by the Moon and the Sun. The influence of other planets in the solar system is small. The value of the gravitational potential at the outer point of the Earth, taking into account tidal effects, depends both on the position of the point in the moving coordinate system and on the relative position of celestial bodies.
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