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関連する概念動画

Types of Collisions - II01:19

Types of Collisions - II

When two or more objects collide with each other, they can stick together to form one single composite object (after collision). The total mass of the object after the collision is the sum of the masses of the original objects, and it moves with a velocity dictated by the conservation of momentum. Although the system's total momentum remains constant, the kinetic energy decreases, and thus such a collision is an inelastic collision. Most of the collisions between objects in daily life are...
Global Climate Change01:50

Global Climate Change

Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
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...
Conditions on Early Earth02:06

Conditions on Early Earth

Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
Conditions on Early Earth02:06

Conditions on Early Earth

Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
Gravimetry: Inorganic And Organic Precipitating Agents00:49

Gravimetry: Inorganic And Organic Precipitating Agents

In gravimetry, the precipitant is chosen carefully to obtain a pure solid that can be easily filtered. Common inorganic precipitants can be used to determine several cations and anions. In some cases, the formation of the same precipitate can be used to determine the cation and the anion. For example, the reaction of barium and chromate ions to give barium chromate is used to determine both barium and chromate. However, precipitates such as hydroxides, oxalates, and metal ammonium phosphates...

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関連する実験動画

Updated: Jul 12, 2026

Laboratory Drop Towers for the Experimental Simulation of Dust-aggregate Collisions in the Early Solar System
09:44

Laboratory Drop Towers for the Experimental Simulation of Dust-aggregate Collisions in the Early Solar System

Published on: June 5, 2014

落ちる星を捕まえる:隕石と古い氷

I M Whillans, W A Cassidy

    Science (New York, N.Y.)
    |October 7, 1983
    PubMed
    まとめ

    新しいモデルによると,南極の青い氷の地域では,隕石が着実に集中している. この研究は,恒常的な隕石の流入と氷の流れを示し,地球上で最も古い氷の配列を潜在的に明らかにしています.

    科学分野:

    • 隕石学と惑星科学について
    • 氷河学 氷河学とは
    • 南極研究南極研究

    背景:

    • 南極の青い氷の地域は,隕石の天然の罠として機能します.
    • 隕石の蓄積を理解するには,氷の流れと蓄積率のモデルが必要です.
    • 以前の研究では,隕石の流入を推定しましたが,濃縮プロセスに関する包括的なモデルはありませんでした.

    研究 の 目的:

    • 南極の青氷地域における隕石の濃度モデルを開発する.
    • 隕石の流入率と露出氷の年齢を推定する.
    • 恒常的な隕石の流入と氷河の流れの仮定を検証するために.

    主な方法:

    • アランヒルズ地域からのデータに基づいて数学的モデルが開発されました.
    • 恒常的な隕石の流入と氷河の流れ率の仮定が適用されました.
    • 隕石の流入と氷の被曝年齢を決定するために計算が行われました.

    主要な成果:

    • このモデルは,隕石の流入量を60 x 10^-6 kg/km^2/yearと推定しています.
    • アランヒルズの近くの露出氷の年齢は0から60万年です.
    • 結果は,流入と隕石の地上の年齢の独立した推定値と一致しています.

    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

    Laser-Induced Fluorescence Emission (L.I.F.E.) as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats
    13:38

    Laser-Induced Fluorescence Emission (L.I.F.E.) as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats

    Published on: October 26, 2019

    関連する実験動画

    Last Updated: Jul 12, 2026

    Laboratory Drop Towers for the Experimental Simulation of Dust-aggregate Collisions in the Early Solar System
    09:44

    Laboratory Drop Towers for the Experimental Simulation of Dust-aggregate Collisions in the Early Solar System

    Published on: June 5, 2014

    Scattering And Absorption of Light in Planetary Regoliths
    11:34

    Scattering And Absorption of Light in Planetary Regoliths

    Published on: July 1, 2019

    Laser-Induced Fluorescence Emission (L.I.F.E.) as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats
    13:38

    Laser-Induced Fluorescence Emission (L.I.F.E.) as Novel Non-Invasive Tool for In-Situ Measurements of Biomarkers in Cryospheric Habitats

    Published on: October 26, 2019

    結論:

    • この発見は,この地域の恒定状態の隕石流入と氷河流の仮定を裏付けている.
    • この研究は,発見された最も古い連続した層状の氷の配列の可能性のある証拠を提示しています.
    • この地域における東南極の氷床は,長期にわたって安定している可能性が高い.