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関連する概念動画

Projectile Motion01:20

Projectile Motion

An object thrown in the air follows a parabolic path under the influence of Earth's gravitational force. The motion of such an object is called projectile motion, and the object itself a projectile. The parabolic path followed by the projectile is called the trajectory. Some common examples of projectile motion are the launching of fireworks, a golf ball in the air, meteors entering the Earth's atmosphere, and the firing of bullets.
When an object falls under gravity and has no horizontal...
Projectile Motion: Example01:18

Projectile Motion: Example

The theory of projectile motion is very useful for players of several sports to improve their performance. For example, a javelin thrower needs to throw their javelin in such a way that it travels as far as possible. The javelin thrower takes a short run-up to increase the initial speed of the javelin. The range of a projectile is at its maximum at a 45° angle so javelin throwers try to angle their throw as close to 45° as possible.
When we speak of the range (R) of a projectile on level...
Impulse01:13

Impulse

According to Newton’s second law of motion, the rate of change of the momentum of an object is the net external force acting on it. The total change in momentum between two timepoints thus depends on both the external force acting on it and the time over which it acts. Describing this mathematically, the total change of an object’s motion is proportional to the force vector and the time over which it is applied. This product is called impulse.
Additionally, it can be shown that the total...
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...
Quarrying of Stone01:15

Quarrying of Stone

Quarrying is the process of extracting stone from a quarry, where specialized techniques are employed to remove large blocks of stone safely and efficiently. This process can involve controlled explosions or more precision-oriented methods such as cutting and drilling.
One common method involves using a diamond belt saw to cut large blocks from the quarry face. These blocks can be about 50 feet long and 12 feet high. After the initial vertical cut, drilling is performed at the base of the block.
Projectile Motion01:25

Projectile Motion

Projectile motion models the flight of an object launched into the air, such as a soccer ball kicked during a penalty, under the simplifying assumption that air resistance is negligible. When gravity is the only force, the object experiences a steady downward acceleration at all times. This single fact explains why projectile motion can be analyzed as two independent motions happening simultaneously: a horizontal motion that does not speed up or slow down, and a vertical motion that continually...

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High-speed Particle Image Velocimetry Near Surfaces
11:59

High-speed Particle Image Velocimetry Near Surfaces

Published on: June 24, 2013

火星隕石の打ち上げ:小さなクレーターからの高速噴出物.

James N Head1, H Jay Melosh, Boris A Ivanov

  • 1Department of Planetary Sciences, University of Arizona, 1629 East University Boulevard, Tucson, AZ 85721, USA.

Science (New York, N.Y.)
|November 9, 2002
PubMed
まとめ

コンピューター・シミュレーションにより, ~3kmの小さなクレーターは,火星の隕石を地球に放出することが明らかになった. この発見は,以前の推定値に異議を唱え,収集された火星隕石で観察された年齢バイアスを説明します.

科学分野:

  • 惑星科学は惑星科学である.
  • インパクトクラテリング (インパクトクラテリング)
  • 地質物理学 地質物理学とは地質物理学です.

背景:

  • 地球で見つかった火星の隕石は,地球の歴史についての洞察を提供します.
  • 火星の岩石の放出メカニズムを理解することは,隕石のコレクションの解釈に不可欠です.

研究 の 目的:

  • 火星からの断片を地球に放出するために必要な最小の衝突クレーターサイズを調査する.
  • 標的物質の性質が隕石の噴出にどのように影響するかを判断する.

主な方法:

  • 火星の地形のアナログの衝突イベントの高解像度のコンピュータシミュレーション.
  • 衝突で発生するレゴリットを含む,均質で層状の標的材料のモデリング.

主要な成果:

  • およそ3キロメートルの小さなクレーターは,地上の隕石の収集を説明するために十分な断片 (10 ^ 7デシメーターの大きさ) を放出することができます.
  • 最小の噴出クレーターの大きさは,以前に推定されたより大幅に小さく,標的物質の組成に依存しています.
  • 層状の地形,特にレゴリットのような弱い表面層を持つ地形は,隕石の噴出のためにより大きな衝撃を必要とします.

結論:

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High-Speed Optical Diagnostics of a Supersonic Ping-Pong Cannon

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関連する実験動画

Last Updated: Jul 13, 2026

High-speed Particle Image Velocimetry Near Surfaces
11:59

High-speed Particle Image Velocimetry Near Surfaces

Published on: June 24, 2013

A Method for Studying the Temperature Dependence of Dynamic Fracture and Fragmentation
09:12

A Method for Studying the Temperature Dependence of Dynamic Fracture and Fragmentation

Published on: June 28, 2015

High-Speed Optical Diagnostics of a Supersonic Ping-Pong Cannon
05:40

High-Speed Optical Diagnostics of a Supersonic Ping-Pong Cannon

Published on: March 24, 2023

  • 衝突シミュレーションは,火星の隕石の噴射ダイナミクスの新しい理解を提供します.
  • この発見は,地上のコレクションにある火星の隕石は,地形の特徴により,地質学的に若い年齢に偏っていることを示唆している.
  • この研究は,シミュレーションの結果と,火星の隕石収集から得られた観測データとを一致させています.