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相关概念视频

Rocket Propulsion in Empty Space - I01:13

Rocket Propulsion in Empty Space - I

The driving force for the motion of any vehicle is friction, but in the case of rocket propulsion in space, the friction force is not present. The motion of a rocket changes its velocity (and hence its momentum) by ejecting burned fuel gases, thus causing it to accelerate in the direction opposite to the velocity of the ejected fuel. In this situation, the mass and velocity of the rocket constantly change along with the total mass of ejected gases. Due to conservation of momentum, the rocket's...
Rocket Propulsion In Empty Space - II01:12

Rocket Propulsion In Empty Space - II

The motion of a rocket is governed by the conservation of momentum principle. A rocket's momentum changes by the same amount (with the opposite sign) as the ejected gases. As time goes by, the rocket's mass (which includes the mass of the remaining fuel) continuously decreases, and its velocity increases. Therefore, the principle of conservation of momentum is used to explain the dynamics of a rocket's motion. The ideal rocket equation gives the change in velocity that a rocket experiences by...
Acceleration due to Gravity on Other Planets01:24

Acceleration due to Gravity on Other Planets

The gravitational acceleration of an object near the Earth's surface is called the acceleration due to gravity. It can be measured by conducting simple experiments on Earth. However, such an experiment is impossible to conduct on the surface of other planets.
Astronomical observations are thus used to measure the acceleration due to gravity on other planets. This can be determined by observing the effect of a planet's gravity on objects close to it. The crucial factor that helps in this...
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,...
Flame Photometry: Lab01:16

Flame Photometry: Lab

In a flame photometer, when a solution like potassium chloride is aspirated into the flame, the solvent evaporates, leaving behind dehydrated salt. This salt dissociates into free gaseous atoms in their ground state. Some of these atoms absorb energy from the flame, leading to their excitation. The excited atoms return to the ground state, emitting photons at characteristic wavelengths. Because only electronic transitions are involved, the resulting emission lines are very narrow. The intensity...
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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相关实验视频

Updated: Jun 30, 2026

Bringing the Visible Universe into Focus with Robo-AO
10:35

Bringing the Visible Universe into Focus with Robo-AO

Published on: February 12, 2013

一个火星年:维京着陆器的成像观测.

K L Jones, R E Arvidson, E A Guinness

    Science (New York, N.Y.)
    |May 25, 1979
    PubMed
    概括

    维京登陆器观察到火星表面的变化,包括冰凝析物形成和来自尘埃的侵蚀率低于预期. 这些发现为火星环境动态提供了洞察力.

    科学领域:

    • 行星科学 行星科学
    • 火星的探索火星的探索
    • 天文地质学 天文地质学

    背景情况:

    • 维京号任务的目的是研究火星表面和大气.
    • 以前对火星表面侵蚀率的估计是基于有限的维京前数据.

    研究的目的:

    • 为了记录火星表面在整个火星一年的变化.
    • 评估维京前侵蚀率预测的准确性.

    主要方法:

    • 使用维京1号和维京2号着陆器的成像系统.
    • 持续数据采集和图像和气象数据的传输.

    主要成果:

    • 在冬季维京2站点观察到固体水 (H2O) 和二氧化碳 (CO2) 凝结物的形成.
    • 有证据表明,由于尘埃再分配,火星表面侵蚀率低于此前预测的水平.

    结论:

    • 火星表面的过程,如凝析物形成和尘埃再分配,表现出季节性变化.
    • 维京登陆器的观测提供了关键的现场数据,用于改进火星表面动态模型.

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    Bringing the Visible Universe into Focus with Robo-AO
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    Published on: February 12, 2013

    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

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    Published on: July 30, 2020