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関連する概念動画

Magnetostatic Boundary Conditions01:28

Magnetostatic Boundary Conditions

An electric field suffers a discontinuity at a surface charge. Similarly, a magnetic field is discontinuous at a surface current. The perpendicular component of a magnetic field is continuous across the interface of two magnetic mediums. In contrast, its parallel component, perpendicular to the current, is discontinuous by the amount equal to the product of the vacuum permeability and the surface current. Like the scalar potential in electrostatics, the vector potential is also continuous...
Elastic Strain Energy for Shearing Stresses01:20

Elastic Strain Energy for Shearing Stresses

As discussed in previous lessons, strain energy in a material is the energy stored when it is elastically deformed, a concept crucial in materials science and mechanical engineering. This energy results from the internal work done against the cohesive forces within the material. When a material undergoes shearing stress and corresponding shearing strain, the strain energy density, which is the energy stored per unit volume, is calculated. Within the elastic limit, where the stress is...
Measuring Acceleration Due to Gravity01:12

Measuring Acceleration Due to Gravity

Consider a coffee mug hanging on a hook in a pantry. If the mug gets knocked, it oscillates back and forth like a pendulum until the oscillations die out.
A simple pendulum can be described as a point mass and a string. Meanwhile, a physical pendulum is any object whose oscillations are similar to a simple pendulum, but cannot be modeled as a point mass on a string because its mass is distributed over a larger area. The behavior of a physical pendulum can be modeled using the principles of...
Impact Loading01:19

Impact Loading

Impact loading occurs when a moving object collides with a stationary structure, such as a rod with a uniform cross-sectional area fixed at one end. Under these conditions, the rod absorbs the kinetic energy from the striking object, leading to deformation and subsequent stress development. As the rod returns to its original position and reaches maximum stress, the absorbed energy, initially manifested as kinetic energy, transforms entirely into strain energy.
In cases of elastic deformation,...
Modes of Standing Waves - I01:03

Modes of Standing Waves - I

A close look at earthquakes provides evidence for the conditions appropriate for resonance, standing waves, and constructive and destructive interference. A building may vibrate for several seconds with a driving frequency matching the building's natural frequency of vibration; this produces a resonance that results in one building collapsing while the neighboring buildings do not. Often, buildings of a certain height are devastated, while other taller buildings remain intact. This phenomenon...
Elastic Strain Energy for Normal Stresses01:22

Elastic Strain Energy for Normal Stresses

Strain energy quantifies the energy stored within a material due to deformation under loading conditions, a fundamental concept in materials science and engineering. The strain energy can be modeled when a material is subjected to axial loading with uniformly distributed stress. In this scenario, the stress experienced by the material is the internal force divided by the cross-sectional area, and the strain induced is directly proportional to this stress through the modulus of elasticity.
If...

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関連する実験動画

Updated: Jul 12, 2026

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
06:55

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling

Published on: August 5, 2016

スティックスリップと地震のソースパラメータ

T Johnson, F T Wu, C H Scholz

    Science (New York, N.Y.)
    |January 19, 1973
    PubMed
    まとめ

    実験室でのスティック・スリップ摩擦実験では,粒子の速度と破裂速度が地震観測と一致していることが明らかになった. このダイナミックな類似性は,スティック・スリップが浅い地震の主なメカニズムであることを強く示唆しています.

    科学分野:

    • 地質物理学 地質物理学とは地質物理学です.
    • 地震学 地震学とは
    • 摩擦物理学 摩擦物理学とは

    背景:

    • 地震は複雑な現象であり,その背後にある物理的メカニズムが積極的に研究されている.
    • 浅瀬地震の発生を理解することは,地震の危険性評価に不可欠です.

    研究 の 目的:

    • 浅瀬地震を制御する物理的プロセスを調査する.
    • 実験室で観測されたスティック・スリップ摩擦現象が地震のダイナミクスを模倣するかどうかを判断する.

    主な方法:

    • スティック・スリップ摩擦イベントのソースパラメータを測定する実験室での実験.
    • 粒子と破裂の拡散速度を分析する.
    • 地震源理論と地震観測との比較.

    主要な成果:

    • スティック・スリップ摩擦現象は,地震の粒子の速度に匹敵する粒子の速度を示します.
    • 実験室での破裂伝播速度は,地震で観測された速度と一致しています.
    • 実験室での棒の滑りと自然発生の地震の間に動的類似性が観察されました.

    結論:

    関連する実験動画

    Last Updated: Jul 12, 2026

    Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
    06:55

    Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling

    Published on: August 5, 2016

  • この発見は,スティック・スリップ摩擦が浅い地震の原因となる支配的なメカニズムであることを示す強力な証拠を提供します.
  • 実験室でのシミュレーションは,地震の断裂の物理学の貴重な洞察を提供します.
  • ダイナミック類似性は,地震現象を理解するために,実験室での摩擦研究の適用をサポートします.