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Residual Stresses in Bending01:18

Residual Stresses in Bending

In the study of elastoplastic members subjected to bending moments, understanding the loading and unloading phases is crucial for assessing material behavior and structural integrity. During the loading phase, as the bending moment increases, the material initially responds elastically, adhering to Hooke's Law, where stress is directly proportional to strain. When the load exceeds the yield strength, plastic deformation occurs, resulting in permanent strain and deformation that remains even...
Plastic Behavior01:21

Plastic Behavior

A material's elastic behavior is characterized by the disappearance of stress once the load is removed, allowing the material to return to its original state. However, when stress surpasses the yield point, yielding commences, marking the onset of plastic deformation or permanent set. This change from elastic to plastic behavior is influenced by the peak stress value and the duration before the load is removed. An intriguing observation occurs when a specimen is loaded, unloaded, and reloaded.
Types of Impact01:30

Types of Impact

Impacts can be classified in various forms, primarily under two subgroups: central impact and oblique impact. A central impact occurs when two objects collide head-on, possessing opposite velocities aligned along the line of impact. Conversely, an oblique impact occurs when two objects collide at an angle, resulting in a modification of both direction and velocity.
The coefficient of restitution is a metric for understanding the dynamics of impacts. It quantifies the ratio of relative velocity...
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...
Impact01:30

Impact

Impact occurs when two bodies collide, leading to the application of impulsive forces between them. Analyzing impact mechanics involves considering two colliding particles moving along a line known as the line of impact, which passes through their centers and is perpendicular to the contact plane.
When particles with different initial velocities collide, they induce deformation by applying equal and opposite impulses. At the point of maximum deformation, the particles move together with...
Elasticity01:12

Elasticity

Elasticity is the ability of an object to withstand the effects of distortion and to return to its original size and shape once the forces causing deformation are removed. When an elastic material deforms under the action of an external force, it experiences internal resistance to the deformation. However, if no external force is applied, it returns to its original state.
The elasticity of an object can be described by a stress-strain curve, which represents the relationship between stress...

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Related Experiment Video

Updated: Jul 12, 2026

Studying Large Amplitude Oscillatory Shear Response of Soft Materials
06:07

Studying Large Amplitude Oscillatory Shear Response of Soft Materials

Published on: April 25, 2019

Postseismic viscoelastic rebound.

A Nur, G Mavko

    Science (New York, N.Y.)
    |January 18, 1974
    PubMed
    Summary

    Earthquakes cause postseismic deformation, mimicking natural surface changes. This study reveals the asthenosphere

    Area of Science:

    • Geophysics
    • Seismology
    • Rheology

    Background:

    • Earthquakes, modeled as dislocations in the lithosphere over the asthenosphere, generate time-dependent surface deformation.
    • Postseismic deformation observed after large earthquakes resembles this modeled behavior.

    Purpose of the Study:

    • To analyze postseismic deformation following the 1946 Nankaido earthquake.
    • To investigate the rheological properties of the Earth's asthenosphere.

    Main Methods:

    • Modeling of an elastic lithosphere overriding a viscoelastic asthenosphere.
    • Analysis of surface deformation data from the 1946 Nankaido earthquake.

    Main Results:

    • The asthenosphere exhibits a viscosity of 5 x 10^19 poise.

    Related Experiment Videos

    Last Updated: Jul 12, 2026

    Studying Large Amplitude Oscillatory Shear Response of Soft Materials
    06:07

    Studying Large Amplitude Oscillatory Shear Response of Soft Materials

    Published on: April 25, 2019

  • A 50% relaxation of the shear modulus was determined for the asthenosphere.
  • Conclusions:

    • Postseismic deformation provides insights into the rheology of the Earth's upper mantle.
    • Large thrust earthquakes can serve as a novel method for rheological exploration.