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Videos de Conceptos Relacionados

IR Spectrum Peak Splitting: Symmetric vs Asymmetric Vibrations01:08

IR Spectrum Peak Splitting: Symmetric vs Asymmetric Vibrations

Identical bonds within a polyatomic group can stretch symmetrically (in-phase) or asymmetrically (out-of-phase). Similar to hydrogen bonding, these vibrations also influence the shape of the IR peak. Generally, asymmetric stretching frequencies are higher than symmetric stretching frequencies. For example, primary amines exhibit two distinct IR peaks between 3300–3500 cm−1 corresponding to the symmetric and asymmetric N-H stretching, while secondary amines exhibit a single stretching vibration...
Torsional Pendulum01:09

Torsional Pendulum

A torsional pendulum involves the oscillation of a rigid body in which the restoring force is provided by the torsion in the string from which the rigid body is suspended. Ideally, the string should be massless; practically, its mass is much smaller than the rigid body's mass and is neglected.
As long as the rigid body's angular displacement is small, its oscillation can be modeled as a linear angular oscillation. The amplitude of the oscillation is an angle. The role of mass is played by the...
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...
Forced Oscillations01:06

Forced Oscillations

When an oscillator is forced with a periodic driving force, the motion may seem chaotic. The motions of such oscillators are known as transients. After the transients die out, the oscillator reaches a steady state, where the motion is periodic, and the displacement is determined.
Shock Waves01:16

Shock Waves

While deriving the Doppler formula for the observed frequency of a sound wave, it is assumed that the speed of sound in the medium is greater than the source's speed through it. When this condition is breached, a shock wave occurs.
When the source's speed approaches the speed of sound, constructive interference between successive wavefronts emitted by the source occurs immediately behind it. Initially, scientists believed that this constructive interference would result in such high pressures...
Atomic Nuclei: Larmor Precession Frequency01:11

Atomic Nuclei: Larmor Precession Frequency

The earth's gravitational field produces a 'twisting force' perpendicular to the angular momentum of a spinning mass (such as a spinning top) that causes the mass to 'wobble' around the gravitational field axis in a phenomenon called precession. Similarly, the magnetic moment (μ) of a spinning nucleus precesses due to an external magnetic field directed along the z-axis. The precession of the magnetic moment vector about the magnetic field is called Larmor precession, and the angular frequency...

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Updated: Jul 13, 2026

Magnetic Resonance Derived Myocardial Strain Assessment Using Feature Tracking
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Magnetic Resonance Derived Myocardial Strain Assessment Using Feature Tracking

Published on: February 13, 2011

El movimiento diferencial del núcleo interno confirmado por la forma de onda del terremoto dobla los dobles.

Jian Zhang1, Xiaodong Song, Yingchun Li

  • 1Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, USA.

Science (New York, N.Y.)
|August 27, 2005
PubMed
Resumen

El núcleo interno de la Tierra gira más rápido que el manto y la corteza. El análisis de las ondas sísmicas que pasan a través del núcleo interno confirma esta rotación, estimada en 0,3 a 0,5 grados por año.

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Área de la Ciencia:

  • La geofísica es la geofísica.
  • Sismología Sismología Sismología.
  • Ciencias de la Tierra Ciencias de la Tierra Ciencias de la Tierra

Sus antecedentes:

  • Las propiedades del núcleo interno de la Tierra son difíciles de estudiar.
  • Las ondas sísmicas que atraviesan el núcleo interno proporcionan información sobre su dinámica.

Objetivo del estudio:

  • Para analizar los cambios temporales en los tiempos de viaje de las ondas sísmicas.
  • Para confirmar la rotación del núcleo interno de la Tierra en relación con el manto y la corteza.

Principales métodos:

  • Análisis de 18 dobles de forma de onda de alta calidad de la región de las Islas Sandwich del Sur.
  • Seguimiento de señales sísmicas (PKP(DF)) que han pasado a través del núcleo interno.
  • Utilizando datos de 58 estaciones en y cerca de Alaska para observar las variaciones en el tiempo de viaje.

Principales resultados:

  • Se observaron cambios temporales consistentes en los tiempos de viaje de las ondas sísmicas.
  • Se observaron diferencias en las codas de onda PKP (DF).
  • El estudio confirmó que el núcleo interno de la Tierra está girando más rápido que el manto y la corteza.

Conclusiones:

  • La rotación del núcleo interno de la Tierra se confirma en aproximadamente 0.3 a 0.5 grados por año.
  • El análisis del doble de la forma de onda mitiga efectivamente los problemas de las localizaciones erróneas de los terremotos y las heterogeneidades a pequeña escala.