太陽系初期の不安定性は,ガス状の円盤の分散によって引き起こされた
Beibei Liu1,2, Sean N Raymond3, Seth A Jacobson4
1Zhejiang Institute of Modern Physics, Department of Physics & Zhejiang University-Purple Mountain Observatory Joint Research Center for Astronomy, Zhejiang University, Hangzhou, China. bbliu@zju.edu.cn.
Nature
|April 28, 2022
まとめ
太陽系の巨大惑星は 初期のガス状円盤の分散により不安定になった可能性が高い. 形成から数百万年後に起こったこの出来事は,火星の小さな大きさを含む地上の惑星の発展を形作ったのかもしれない.
科学分野:
- 惑星科学
- 天体物理学
- 計算による天体物理学
背景:
- 太陽系の軌道構造は 巨大な惑星の動的不安定性によるものです
- この不安定性の正確な引き金とタイミングは 未定です
研究 の 目的:
- 巨大惑星の不安定性を引き起こす ガス状の原始惑星円盤の分散を調査する
- 太陽系初期の大惑星の 不安定のタイミングを 決定するために
主な方法:
- ダイナミックシミュレーション 巨大惑星の移動と不安定さ
- 原惑星円盤の進化の水力学モデル.
主要な成果:
- 巨大な惑星の不安定さは ガス状の円盤が内側から外側へ 散らばったことによって引き起こされたようです
- 蒸発する円盤の内縁は 惑星の軌道を乱し 動的圧縮と不安定を引き起こしました
- シミュレートされた最終的な惑星の軌道は観測された太陽系の構成と一致する.
結論:
- 巨大惑星の不安定さは 太陽系の誕生から数百万年後の ガス状の円盤の消散時に発生した.
- 初期の巨大惑星の不安定さは,地上の惑星の形成に影響を与え,火星の質量を彫刻したのかもしれない.
関連する概念動画
Kepler's First Law of Planetary Motion
4.3K
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,...
4.3K
Distribution and Dispersion
22.5K
To understand intra-specific interactions in populations, scientists measure the spatial arrangement of species individuals. This geographic arrangement is known as the species distribution or dispersion. Highly territorial species exhibit a uniform distribution pattern, in which individuals are spaced at relatively equal distances from one another. Species that are highly tied to particular resources, such as food or shelter, tend to concentrate around those resources, and thus exhibit a...
22.5K
Kepler's Second Law of Planetary Motion
4.5K
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...
4.5K
Kepler's Third Law of Planetary Motion
3.6K
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...
3.6K
Reduced Mass Coordinates: Isolated Two-body Problem
1.6K
In classical mechanics, the two-body problem is one of the fundamental problems describing the motion of two interacting bodies under gravity or any other central force. When considering the motion of two bodies, one of the most important concepts is the reduced mass coordinates, a quantity that allows the two-body problem to be solved like a single-body problem. In these circumstances, it is assumed that a single body with reduced mass revolves around another body fixed in a position with an...
1.6K
Second Order systems II
180
In an underdamped second-order system, where the damping ratio ζ is between 0 and 1, a unit-step input results in a transfer function that, when transformed using the inverse Laplace method, reveals the output response. The output exhibits a damped sinusoidal oscillation, and the difference between the input and output is termed the error signal. This error signal also demonstrates damped oscillatory behavior. Eventually, as the system reaches a steady state, the error diminishes to zero.
180


