论文标题
质量转移的月球中心的理论和计算以及远处和靠近月球侧面的地壳厚度差异
A Theory and Calculation of Lunar Center of Mass Shift and the Crustal Thickness Difference Between Far and Near Sides of the Moon
论文作者
论文摘要
自1959年以来，苏联航天器Luna 3自1959年以来，天文学中的远处和靠近月球侧面的地壳厚度差异的原因被认为是一个空旷的问题。这个问题称为月球范围高地问题。在本文中，作者推断了月球从几何中心的大规模转移中心，以及远处和附近月球之间的地壳厚度的差异来解释它。尽管还有其他理论来解释这些现象，但该理论将它们解释为自然而然的是由于地球外部重力力以及月球同步旋转和革命而对月球材料的影响而自然产生的。作者的数学模型导致质量移位中心的计算值为1.6 km，地壳厚度差为16 km。作者推论的质量转移和地壳厚度差异的值接近其可接受值的约5％至10％。作者理论的一个意外且可推论的结果是，月球的质量转移中心在月球衰退下以大约1.6 x 10-4 mm/yr的速度降低了月球中心。
The cause for the difference in crustal thickness between the far and near sides of the moon has been considered an open problem in astronomy since 1959 when the Soviet spacecraft Luna 3 sent back the first images of the lunar farside. The problem is referred to as the lunar farside highlands problem. In this article, the author deduces the center of mass shift of the moon from its geometrical center and the difference in crustal thickness between the far and near lunar sides necessary to explain it. Although there have been other theories proposed to explain these phenomena, this theory explains them as arising naturally from the effects on lunar material due to the earth's external gravity force and the moon's synchronous rotation and revolution. The author's mathematical model results in a calculated value of 1.6 km for the center of mass shift and a crustal thickness difference of 16 km. The author's deduced values of center of mass shift and crustal thickness difference are close to within about 5 to 10% of their accepted values. One unexpected and deducible result of the author's theory is that the center of mass shift of the moon is decreasing towards moon center under lunar recession at the current rate of about 1.6 x 10-4 mm/yr.
