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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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Related Experiment Video

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

Microseisms: mode structure and sources.

M N Toksöz, R T Lacoss

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

    Microseisms, seismic waves from atmospheric storms, were studied using seismometers. Researchers identified body and surface waves, pinpointing storm sources from wave patterns.

    Area of Science:

    • Seismology
    • Earthquake Science
    • Atmospheric Physics

    Background:

    • Microseisms are continuous seismic wave vibrations.
    • Their sources are linked to oceanic wave activity and atmospheric pressure systems.

    Purpose of the Study:

    • To analyze the frequency-wave number spectra of microseisms.
    • To identify the types of seismic waves constituting microseisms.
    • To determine the geographical origins of microseismic activity.

    Main Methods:

    • Utilized short-period and long-period seismometers at the Large Aperture Seismic Array (LASA).
    • Analyzed frequency-wave number spectra of microseisms.
    • Determined phase velocity and direction of body waves.

    Main Results:

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    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

    Related Experiment Videos

    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

    • Short-period microseisms (<5s) include body waves and higher-mode surface waves.
    • Body wave analysis identified source areas correlating with low-pressure weather systems.
    • Longer-period microseisms are dominated by fundamental-mode Rayleigh and Love waves.
    • Microseismic energy predominantly arrived from the northeast and west at LASA.

    Conclusions:

    • Microseisms provide valuable data for tracking atmospheric disturbances.
    • The study successfully differentiated wave types and located microseism sources.
    • Seismic wave analysis offers a method for remote sensing of weather phenomena.