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Microcracking in Concrete

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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...
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A wave is a disturbance that propagates from its source, repeating itself periodically, and is typically associated with simple harmonic motion. Mechanical waves are governed by Newton's laws and require a medium to travel. A medium is a substance in which a mechanical wave propagates, and the medium produces an elastic restoring force when it is deformed.
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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...
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The total energy associated with a wavelength is the sum of the potential energy and the kinetic energy. The average rate of energy transfer associated with a wave is called its power, which is total energy divided by the time it takes to transfer the energy. For a sinusoidal wave, energy and power are proportional to the square of both the amplitude and the angular frequency.
Waves can also be concentrated or spread out, as characterized by the intensity of the wave. Intensity is directly...
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Updated: Mar 15, 2026

Microparticle Manipulation by Standing Surface Acoustic Waves with Dual-frequency Excitations
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Microsismos de ondas telesísmicas S

Kiwamu Nishida1, Ryota Takagi2

  • 1Earthquake Research Institute, University of Tokyo, 1-1-1 Yayoi 1, Bunkyo-ku, Tokyo 113-0032, Japan. knishida@eri.u-tokyo.ac.jp.

Science (New York, N.Y.)
|August 27, 2016
PubMed
Resumen
Este resumen es generado por máquina.

Los investigadores rastrearon los microseismos de las tormentas distantes utilizando matrices sísmicas. Observaron ondas P y S, pero las ondas S polarizadas horizontalmente (ondas SH) siguen sin ser explicadas por los modelos actuales, ofreciendo nuevos conocimientos sobre la Tierra

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Área de la Ciencia:

  • Sismología
  • La oceanografía
  • La geofísica

Sus antecedentes:

  • Los microseismos, las vibraciones de las ondas sísmicas, son generados por las olas del océano.
  • El seguimiento de las ubicaciones de las fuentes de microseismos es crucial para comprender los mecanismos de excitación.

Objetivo del estudio:

  • Investigar las ubicaciones de las fuentes y la partición de energía de los componentes de las ondas sísmicas (ondas P y S) de los microseismos.
  • Para entender los mecanismos de excitación de los micro sismos generados por las tormentas distantes.

Principales métodos:

  • Utilizó una matriz sísmica en Japón para observar microseismos.
  • Analizó los microseismos de ondas P y S originados por una severa tormenta en el Océano Atlántico.

Principales resultados:

  • Las ondas P observadas y las ondas S polarizadas verticalmente (ondas SV) son consistentes con el forzamiento de oleaje no lineal del océano.
  • Se han observado ondas S polarizadas horizontalmente (ondas SH) que no se explican con los modelos actuales de la Tierra unidimensional.

Conclusiones:

  • Los modelos actuales explican adecuadamente los microsismos de ondas P y SV, pero no tienen en cuenta las ondas SH.
  • Las ubicaciones precisas de las fuentes de microseismos pueden crear potencialmente un nuevo catálogo para explorar el interior de la Tierra.