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関連する概念動画

Kepler's First Law of Planetary Motion01:10

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,...
Kepler's Third Law of Planetary Motion01:18

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...
Kepler's Second Law of Planetary Motion01:29

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...
Variation in Acceleration due to Gravity near the Earth's Surface01:20

Variation in Acceleration due to Gravity near the Earth's Surface

An object's apparent weight is its weight measured by a spring balance at its location. It is different from its true weight, the force with which the Earth pulls it, because of the Earth's rotation. Mathematically, an object's apparent weight equals its true weight minus the centripetal force that keeps it in a circular motion along with the Earth's surface every 24 hours.
The difference between the true and apparent weights is proportional to the square of the Earth's angular speed. Since the...
Circular Orbits and Critical Velocity for Satellites01:16

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...
Impact: Problem Solving01:26

Impact: Problem Solving

In an experiment conducted during a Mars mission, a rover propels a projectile with an initial velocity, and the projectile rebounds after colliding with the Martian surface. To ascertain the maximum height attained by the projectile after this collision, the known restitution coefficient and acceleration due to gravity are employed.
By designating the launch point as the origin and utilizing kinematic equations, the vertical component of the projectile's velocity at the point of impact is...

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関連する実験動画

Updated: Jul 12, 2026

Surface Mapping of Earth-like Exoplanets using Single Point Light Curves
06:48

Surface Mapping of Earth-like Exoplanets using Single Point Light Curves

Published on: May 10, 2020

マジェラン:金星の表面改変の初期分析

R E Arvidson, V R Baker, C Elachi

    Science (New York, N.Y.)
    |April 12, 1991
    PubMed
    まとめ

    マジェランによる最初の観測は,惑星の存在を示している.

    科学分野:

    • 惑星科学は惑星科学である.
    • 地質学 地質学 地質学
    • 大気科学 大気科学

    背景:

    • 惑星の表面の進化を理解することは,比較惑星学にとって極めて重要です.
    • マジェランミッションのデータは,金星の表面プロセスに関する高解像度の洞察を提供します.

    研究 の 目的:

    • 特定の惑星の地質学的および大気学的過程の証拠をマジェランのデータを分析するために.
    • 表面の特徴と材料の分布を特徴づけるために.

    主な方法:

    • マジェランのレーダー画像と高度測定データの分析.
    • 表面処理を推論するために,地形および質感の変動の解釈.

    主要な成果:

    • 高い介電常数を持つ材料は,高さや急さのある地域に集中しています.
    • 広範囲にわたる噴出堆積物は,大きな衝突クレーター形成を示している.
    • 風に吹き込まれた堆積物は,特定の場所での活発なエオリア過程を示唆しています.
    • 証拠は,大気相互作用と質量損失による漸進的な表面劣化を示しています.

    結論:

    さらに関連する動画

    Scattering And Absorption of Light in Planetary Regoliths
    11:34

    Scattering And Absorption of Light in Planetary Regoliths

    Published on: July 1, 2019

    Selective Area Modification of Silicon Surface Wettability by Pulsed UV Laser Irradiation in Liquid Environment
    08:48

    Selective Area Modification of Silicon Surface Wettability by Pulsed UV Laser Irradiation in Liquid Environment

    Published on: November 9, 2015

    関連する実験動画

    Last Updated: Jul 12, 2026

    Surface Mapping of Earth-like Exoplanets using Single Point Light Curves
    06:48

    Surface Mapping of Earth-like Exoplanets using Single Point Light Curves

    Published on: May 10, 2020

    Scattering And Absorption of Light in Planetary Regoliths
    11:34

    Scattering And Absorption of Light in Planetary Regoliths

    Published on: July 1, 2019

    Selective Area Modification of Silicon Surface Wettability by Pulsed UV Laser Irradiation in Liquid Environment
    08:48

    Selective Area Modification of Silicon Surface Wettability by Pulsed UV Laser Irradiation in Liquid Environment

    Published on: November 9, 2015

  • 惑星の表面は,衝突,エオリア,および退廃の過程の複雑な相互作用を示しています.
  • 材料の分布は地形と潜在的に大気動力学の影響を受けます.
  • 進行中の表面改変は,ダイナミックな地質的および大気の環境を示唆しています.