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関連する概念動画

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...
Scanning Electron Microscopy01:07

Scanning Electron Microscopy

A scanning electron microscope (SEM) is used to study the surface features of a sample by using an electron beam that scans the sample surface in a two-dimensional manner. Typically, areas between ~1 centimeter to 5 micrometers in width can be imaged. SEM can be used to image bacteria, viruses, tissues as well as larger samples like insects. Conventional SEM gives a magnification ranging from 20X to 30,000X and spatial resolution of 50 to 100 nanometers.
Fundamental Principles
Accelerated...
Microcracking in Concrete01:20

Microcracking in Concrete

Microcracking in concrete refers to the tiny cracks that can form within the material even before any external load is applied. These microcracks typically occur at the interface between the coarse aggregate and the hydrated cement paste, often as a result of differential volume changes prompted by variations in stress-strain behavior, as well as thermal and moisture movement. Initially, these microcracks remain stable and do not grow substantially until the concrete is stressed to about 30...
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...
Overview of Electron Microscopy01:25

Overview of Electron Microscopy

The wavelengths of visible light ultimately limit the maximum theoretical resolution of images created by light microscopes. Most light microscopes can only magnify 1000X, and a few can magnify up to 1500X. Electrons, like electromagnetic radiation, can behave like waves, but with wavelengths of 0.005 nm, they produce significantly greater resolution up to 0.05 nm as compared to 500 nm for visible light. An electron microscope (EM) can create a sharp image that is magnified up to 2,000,000X.
Transmission Electron Microscopy01:15

Transmission Electron Microscopy

In 1931, physicist Ernst Ruska—building on the idea that magnetic fields can direct an electron beam just as lenses can direct a beam of light in an optical microscope—developed the first prototype of the electron microscope. This development led to the development of the field of electron microscopy. In the transmission electron microscope (TEM), electrons are produced by a hot tungsten element and accelerated by a potential difference in an electron gun, which gives them up to 400 keV in...

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関連する実験動画

Updated: Jul 12, 2026

Induction of Microstreaming by Nonspherical Bubble Oscillations in an Acoustic Levitation System
08:19

Induction of Microstreaming by Nonspherical Bubble Oscillations in an Acoustic Levitation System

Published on: May 9, 2021

マイクロシズム:モード構造と発生源

M N Toksöz, R T Lacoss

    Science (New York, N.Y.)
    |February 23, 1968
    PubMed
    まとめ

    マイクロ地震,つまり大気嵐からの地震波は,地震計を使って研究されました. 研究者は,体と表面の波を特定し,波のパターンから嵐の源を特定しました.

    科学分野:

    • 地震学 地震学とは
    • 地震科学 地震科学 地震科学
    • 大気物理学 大気物理学

    背景:

    • マイクロ地震は連続した地震波の振動である.
    • その源は,海洋の波動活動と大気圧システムと結びついている.

    研究 の 目的:

    • 微地震の周波数波数スペクトルを分析するために.
    • マイクロ地震を構成する地震波の種類を特定する.
    • マイクロ地震活動の地理的起源を決定する.

    主な方法:

    • 大開口地震配列 (LASA) で短期および長期の地震計を使用しました.
    • 微地震の周波数波数スペクトルを分析した.
    • 体の波の相速度と方向を決定する.

    主要な成果:

    • 短期間マイクロ地震 (<5秒) には,体波と高モード表面波が含まれます.
    • ボディウェーブ分析により,低圧気象システムと相関する源領域が特定されました.
    • 長い周期の微震は,基本モードのレイリー波とラブ波が支配しています.
    • マイクロ地震エネルギーは,主にLASAの北東と西から到着しました.

    さらに関連する動画

    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

    関連する実験動画

    Last Updated: Jul 12, 2026

    Induction of Microstreaming by Nonspherical Bubble Oscillations in an Acoustic Levitation System
    08:19

    Induction of Microstreaming by Nonspherical Bubble Oscillations in an Acoustic Levitation System

    Published on: May 9, 2021

    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

    結論:

    • マイクロ地震は,大気の乱れを追跡するための貴重なデータを提供します.
    • この研究では,波の種類を区分し,微小地震源を特定することが成功しました.
    • 地震波分析は,気象現象のリモートセンシングのための方法を提供します.