Ward WR, Canup RM
Southwest Research Institute, Boulder, Colorado 80302, USA.
Nature. 2000 Feb 17;403(6771):741-3. doi: 10.1038/35001516.
The Moon is generally believed to have formed from the debris disk created by a large body colliding with the early Earth. Recent models of this process predict that the orbit of the newly formed Moon should be in, or very near, the Earth's equatorial plane. This prediction, however, is at odds with the known history of the lunar orbit: the orbit is currently expanding, but can be traced back in time to reveal that, when the Moon formed, its orbital inclination relative to the Earth's equator was I approximately = 10 degrees. The cause of this initial inclination has been a mystery for over 30 years, as most dynamical processes (such as those that act to flatten Saturn's rings) will tend to decrease orbital inclinations. Here we show that the Moon's substantial orbital inclination is probably a natural result of its formation from an impact-generated disk. The mechanism involves a gravitational resonance between the Moon and accretion-disk material, which can increase orbital inclinations up to approximately 15 degrees.
一般认为,月球是由一个大型天体与早期地球碰撞所产生的碎片盘形成的。最近关于这个过程的模型预测,新形成的月球轨道应该在地球赤道平面内,或者非常接近赤道平面。然而,这一预测与月球轨道的已知历史不符:目前月球轨道正在扩大,但追溯其历史可以发现,月球形成时,其相对于地球赤道的轨道倾角约为10度。30多年来,这种初始倾角的成因一直是个谜,因为大多数动力学过程(比如那些使土星环变平的过程)往往会减小轨道倾角。我们在此表明,月球较大的轨道倾角可能是其由撞击产生的碎片盘形成的自然结果。该机制涉及月球与吸积盘物质之间的引力共振,这种共振可使轨道倾角增大至约15度。