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Spherical integral transforms of second-order gravitational tensor components onto third-order gravitational tensor components

机译:二阶重力张量分量到三阶重力张量分量的球积分变换

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摘要

New spherical integral formulas between components of the second- and third-order gravitational tensors are formulated in this article. First, we review the nomenclature and basic properties of the second- and third-order gravitational tensors. Initial points of mathematical derivations, i.e., the second- and third-order differential operators defined in the spherical local North-oriented reference frame and the analytical solutions of the gradiometric boundary-value problem, are also summarized. Secondly, we apply the third-order differential operators to the analytical solutions of the gradiometric boundary-value problem which gives 30 new integral formulas transforming (1) vertical-vertical, (2) vertical-horizontal and (3) horizontal-horizontal second-order gravitational tensor components onto their third-order counterparts. Using spherical polar coordinates related sub-integral kernels can efficiently be decomposed into azimuthal and isotropic parts. Both spectral and closed forms of the isotropic kernels are provided and their limits are investigated. Thirdly, numerical experiments are performed to test the consistency of the new integral transforms and to investigate properties of the sub-integral kernels. The new mathematical apparatus is valid for any harmonic potential field and may be exploited, e.g., when gravitational/magnetic second- and third-order tensor components become available in the future. The new integral formulas also extend the well-known Meissl diagram and enrich the theoretical apparatus of geodesy.
机译:本文提出了二阶和三阶引力张量各分量之间的新球形积分公式。首先,我们回顾一下二阶和三阶引力张量的命名法和基本性质。还总结了数学推导的起点,即球形局部北向参考系中定义的二阶和三阶微分算子以及梯度法边值问题的解析解。其次,我们将三阶微分算子应用于梯度边值问题的解析解,该问题给出了30个新的积分公式,它们转换了(1)垂直-垂直,(2)垂直-水平和(3)水平-水平第二-将引力张量分量排列到三阶对应物上。使用球形极坐标,可以有效地将相关的子积分核分解为方位角和各向同性的部分。提供了各向同性内核的频谱形式和封闭形式,并研究了它们的极限。第三,进行数值实验,以检验新积分变换的一致性,并研究次积分核的性质。该新的数学装置对于任何谐波势场均有效,并且例如在将来重力/磁性二阶和三阶张量分量可用时可以被利用。新的积分公式还扩展了著名的Meissl图并丰富了大地测量学的理论工具。

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