月球节点潮和距离月球的距离在前坎布里亚时期
1Department of Atmospheric and Oceanic Sciences, The University of Michigan, Ann Arbor 48109, USA.
Nature
|April 17, 1986
概括
研究人员使用前坎布里亚纪带带铁形状来确定古代月球距离. 这一发现支持月球轨道的长期稳定性,并为地球早期的潮演变提供了新的见解.
科学领域:
- 古气候学 古气候学
- 地质物理学 地质物理学
- 月球科学 月球科学
背景情况:
- 以前的潮演变模型表明,在遥远的过去发生了灾难性的地球/月球碰撞,缺乏直接证据.
- 了解古代月球距离对于重建地球早期气候和轨道动态至关重要.
研究的目的:
- 为了直接确定月球距离在前坎布里亚时代.
- 测试月球节点潮影响古代气候模式的假设.
主要方法:
- 对25亿年前澳大利亚带状铁形成 (BIF) 的分析.
- 确定 23.3 ± 0.3 年周期,解释为月球节点潮的签名.
- 根据观察到的周期性计算古代的月球距离.
主要成果:
- 在25亿年前的BIF中,确定了23.3±0.3年的周期性.
- 这种周期性归因于月球节点潮对气候的影响.
- 在25亿年前的月球距离大约是52地球半径.
结论:
- 这些发现提供了第一个直接证据,证明了在甲纪前的月球距离.
- 推断的前坎布里亚时代的潮摩擦历史与古生物学数据和月球轨道稳定性一致.
- 这种方法提供了一种潜在的新方法,通过分析前坎布里亚时代沉积物记录中的米兰科维奇周期来确定古代月球距离.
相关概念视频
Gravity between Spherical Bodies
Newton's law of gravitation describes the gravitational force between any two point masses. However, for extended spherical objects like the Earth, the Moon, and other planets, the law holds with an assumption that masses of spherical objects are concentrated at their respective centers.
This assumption can be proved easily by showing that the expression for gravitational potential energy between a hollow sphere of mass (M) and a point mass (m) is the same as it would be for a pair of extended...
This assumption can be proved easily by showing that the expression for gravitational potential energy between a hollow sphere of mass (M) and a point mass (m) is the same as it would be for a pair of extended...
Circular Orbits and Critical Velocity for Satellites
The Moon orbits around the Earth. In turn, the Earth (and other planets) orbit the Sun. The space directly above our atmosphere is filled with artificial satellites in orbit. One can examine the circular orbit, the simplest kind of orbit, to understand the relationship between the speed and the period of planets and satellites with respect to their positions and the bodies that they orbit.
Nicolaus Copernicus (1473-1543) first suggested that the Earth and all other planets orbit the Sun in...
Nicolaus Copernicus (1473-1543) first suggested that the Earth and all other planets orbit the Sun in...
Kepler's First Law of Planetary Motion
In the early 17th century, German astronomer and mathematician Johannes Kepler postulated three laws for the motion of planets in the solar system. He formulated his first two laws based on the observations of his forebears, Nikolaus Copernicus and Tycho Brahe.
Polish astronomer Nikolaus Copernicus put forth a theory that stated a heliocentric model for the solar system. According to this heliocentric theory, all the planets, including Earth, orbit the Sun in circular orbits.
On the other hand,...
Polish astronomer Nikolaus Copernicus put forth a theory that stated a heliocentric model for the solar system. According to this heliocentric theory, all the planets, including Earth, orbit the Sun in circular orbits.
On the other hand,...
Kepler's Second Law of Planetary Motion
In the early 17th century, German astronomer and mathematician Johannes Kepler postulated three laws for the motion of planets in the solar system. His first law states that all planets orbit the Sun in an elliptical orbit, with the Sun at one of the ellipse's foci. Therefore, the distance of a planet from the Sun varies throughout its revolution around the Sun.
While in an elliptical orbit, the total energy of the planet is conserved. Therefore, the planet slows down when it is at apogee and...
While in an elliptical orbit, the total energy of the planet is conserved. Therefore, the planet slows down when it is at apogee and...
Kepler's Third Law of Planetary Motion
In the early 17th century, German astronomer and mathematician Johannes Kepler postulated three laws for the motion of planets in the solar system. In 1909, he formulated his first two laws based on the observations of his forebears, Nikolaus Copernicus and Tycho Brahe. However, in 1918, he published his third law of planetary motion, which gives a precise mathematical relationship between a planet's average distance from the Sun and the amount of time it takes to revolve around the Sun. It...
Tidal Forces
The origin of Earth's ocean tides has been a subject of continuous investigation for over 2000 years. However, the work of Newton is considered to be the beginning of the proper understanding of the phenomenon. Ocean tides are the result of gravitational tidal forces. These same tidal forces are present in any astronomical body; they are responsible for the internal heat that creates the volcanic activity on Io, one of Jupiter's moons, and the breakup of stars that get too close to black holes.


