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Damped Oscillations01:07

Damped Oscillations

In the real world, oscillations seldom follow true simple harmonic motion. A system that continues its motion indefinitely without losing its amplitude is termed undamped. However, friction of some sort usually dampens the motion, so it fades away or needs more force to continue. For example, a guitar string stops oscillating a few seconds after being plucked. Similarly, one must continually push a swing to keep a child swinging on a playground.
Although friction and other non-conservative...
Velocity and Acceleration of a Wave00:51

Velocity and Acceleration of a Wave

A wave propagates through a medium with a constant speed, known as a wave velocity. It is different from the speed of the particles of the medium, which is not constant. In addition, the velocity of the medium is perpendicular to the velocity of the wave. The variable speed of the particles of the medium implies that there must be acceleration associated with it. 
The velocity of the particles can be obtained by taking the partial derivative of the position equation with respect to time. We can...
Deriving the Speed of Sound in a Liquid01:09

Deriving the Speed of Sound in a Liquid

As with waves on a string, the speed of sound or a mechanical wave in a fluid depends on the fluid's elastic modulus and inertia. The two relevant physical quantities are the bulk modulus and the density of the material. Indeed, it turns out that the relationship between speed and the bulk modulus and density in fluids is the same as that between the speed and the Young's modulus and density in solids.
The speed of sound in fluids can be derived by considering a mechanical wave propagating...
Relative Motion Analysis using Rotating Axes-Problem Solving01:29

Relative Motion Analysis using Rotating Axes-Problem Solving

Consider a crane whose telescopic boom rotates with an angular velocity of 0.04 rad/s and angular acceleration of 0.02 rad/s2. Along with the rotation, the boom also extends linearly with a uniform speed of 5 m/s. The extension of the boom is measured at point D, which is measured with respect to the fixed point C on the other end of the boom. For the given instant, the distance between points C and D is 60 meters.
Here, in order to determine the magnitude of velocity and acceleration for point...
Distance Problem01:29

Distance Problem

When an object's velocity changes over time, the total distance traveled can be determined by summing small displacement intervals over short increments. This approach approximates the true distance through numerical summation and the use of integral calculus. An estimate of the total displacement can be obtained by measuring velocity at regular intervals and multiplying each value by the corresponding time step.If a runner accelerates over the first three seconds of a race, speed measurements...

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Video Experimental Relacionado

Updated: Jun 30, 2026

Echo Particle Image Velocimetry
16:31

Echo Particle Image Velocimetry

Published on: December 27, 2012

Interferometría de ondas de coda para estimar el comportamiento no lineal en la velocidad sísmica.

Roel Snieder1, Alexandre Grêt, Huub Douma

  • 1Department of Geophysics and Center for Wave Phenomena, Colorado School of Mines, Golden, CO 80401, USA.

Science (New York, N.Y.)
|March 23, 2002
PubMed
Resumen

La interferometría de ondas de Coda utiliza ondas sísmicas dispersas para monitorear los cambios en el medio. Este estudio cuantifica el granito.

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Área de la Ciencia:

  • La geofísica es la geofísica.
  • Sismología Sismología Sismología.
  • Ciencia de los materiales Ciencia de los materiales.

Sus antecedentes:

  • La interferometría de ondas de Coda (CWI) analiza múltiples ondas dispersas.
  • CWI infiere cambios temporales dentro de un medio usando receptores limitados.

Objetivo del estudio:

  • Para determinar la dependencia no lineal de la velocidad sísmica en granito de la temperatura.
  • Para investigar las emisiones acústicas asociadas durante los cambios de temperatura.

Principales métodos:

  • Utilizó la interferometría de ondas de coda para registrar múltiples ondas dispersas.
  • Aplicó la técnica a muestras de granito bajo temperaturas variables.

Principales resultados:

  • Se estableció una relación no lineal entre la velocidad sísmica en granito y la temperatura.
  • Las emisiones acústicas asociadas observadas y cuantificadas.

Conclusiones:

  • La interferometría de ondas de Coda es efectiva para monitorear los cambios de velocidad sísmica en el granito.
  • La técnica puede operar en modos de advertencia o diagnóstico para la detección de cambios en el medio temporal.