用平面椭球盘的势表示天体的重力场

Pub Date : 2023-04-28 DOI:10.15407/knit2023.02.078
M. Fys, A. Brydun, A. Sohor, V..A. Lozynskyy
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引用次数: 0

摘要

在经典势理论的基础上,提出了用平面盘势表示行星外引力场的一种可能方法。同时,利用单层和双层的势进行描述,将积分区放置在赤道平面上。这些函数的级数展开式的系数是引力场斯托克斯常数的线性组合,并且用它们唯一地表示。串联项是单层或双层电位。这使得利用椭球势理论的结果来计算这些项成为可能。与传统的球面函数级数相比,这种级数的收敛范围更广,实际上涵盖了不包括积分区域的外部势的影响,包括曲面的表面部分。由于所得到的展开式不存在收敛性问题,我们可以更充分地解释所得到的结果。构造单层和双层势能的平坦密度分布是研究天体内部结构的一个额外工具,因为它本质上是行星内部体积密度在赤道平面上的投影。因此,这些函数的极值结合了行星内部三维分布函数的特征
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PRESENTATION OF THE GRAVITY FIELD OF CELESTIAL BODIES USING THE POTENTIALS OF FLAT ELLIPSOIDAL DISCS
One of the possible ways for representing the external gravitational field of the planet by the potentials of flat discs, based on the classical potential theory, is proposed. At the same time, the potentials of a single- and double-layer are used for the description with the placement of the integration regions in the equatorial plane. The coefficients of the series expansion of these functions are linear combinations of the Stokes constants of the gravitational field and are uniquely expressed in terms of them. Series terms are single- or double-layer potentials. This makes it possible to calculate these terms using the results of the ellipsoid potential theory. The convergence of such a series, in contrast to the traditional one for spherical functions, is much wider and practically covers the effect of the external potential excluding the region of integration, including in the superficial parts of the surface. Since there is no problem with the convergence of the obtained expansions, we can interpret the obtained results more fully. The construction of flat density distributions for the potentials of a single and double layer is an additional tool in the study of the internal structure of the celestial body, as it is essentially a projection of the volume density of the planet’s interior onto the equatorial plane. Therefore, the extrema of these functions combine the features of the three-dimensional distribution function of the planet’s interior
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