Jove
Visualize
联系我们
JoVE
x logofacebook logolinkedin logoyoutube logo
关于 JoVE
概览领导团队博客JoVE 帮助中心
作者
出版流程编辑委员会范围与政策同行评审常见问题投稿
图书馆员
用户评价订阅访问资源图书馆顾问委员会常见问题
研究
JoVE JournalMethods CollectionsJoVE Encyclopedia of Experiments存档
教育
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab Manual教师资源中心教师网站
使用条款与条件
隐私政策
政策

相关概念视频

Microcracking in Concrete01:20

Microcracking in Concrete

527
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...
527
Travelling Waves01:04

Travelling Waves

7.3K
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.
Water waves, sound waves, and seismic waves are some examples of mechanical waves. For water waves, the wave propagation medium is...
7.3K
Modes of Standing Waves - I01:03

Modes of Standing Waves - I

4.2K
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...
4.2K
Energy and Power of a Wave00:58

Energy and Power of a Wave

5.1K
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...
5.1K

您也可能阅读

相关文章

通过共同作者、期刊和引用图与本文相关的文章。

排序
Same author

Rupture of solidified ancient magma that impeded preceding swarm migrations led to the 2024 Noto earthquake.

Science advances·2025
Same author

The forearc seismic belt: A fluid pathway constraining down-dip megathrust earthquake rupture.

Science (New York, N.Y.)·2025
Same author

Coseismic crustal seismic velocity changes associated with the 2024 M<sub>W</sub> 7.5 Noto earthquake, Japan.

Earth, planets, and space : EPS·2025
Same author

Earth-shaking J. LEAGUE supporters.

Earth, planets, and space : EPS·2022
Same author

Global fast-traveling tsunamis driven by atmospheric Lamb waves on the 2022 Tonga eruption.

Science (New York, N.Y.)·2022
Same author

Atmospheric waves and global seismoacoustic observations of the January 2022 Hunga eruption, Tonga.

Science (New York, N.Y.)·2022
Same journal

Erratum for the Research Article "Detecting supramolecular organic nanoparticles during heat wave".

Science (New York, N.Y.)·2026
Same journal

Local signals, systemic decline.

Science (New York, N.Y.)·2026
Same journal

The mechanics of liver regeneration.

Science (New York, N.Y.)·2026
Same journal

Computing in a memory with physics.

Science (New York, N.Y.)·2026
Same journal

Retraction.

Science (New York, N.Y.)·2026
Same journal

Making time.

Science (New York, N.Y.)·2026
查看所有相关文章

相关实验视频

Updated: Mar 15, 2026

Microparticle Manipulation by Standing Surface Acoustic Waves with Dual-frequency Excitations
06:51

Microparticle Manipulation by Standing Surface Acoustic Waves with Dual-frequency Excitations

Published on: August 21, 2018

7.5K

远距离的S波微震

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
概括
此摘要是机器生成的。

研究人员使用地震阵列追踪远方风暴的微地震. 他们观察到P和S波,但水平偏振的S波 (SH波) 仍然无法通过当前的模型来解释,为地球提供了新的见解

更多相关视频

Investigating the Potential of Singly Curved Thin Piezoelectric Transducers for Energy Harvesting and Structural Health Monitoring
07:02

Investigating the Potential of Singly Curved Thin Piezoelectric Transducers for Energy Harvesting and Structural Health Monitoring

Published on: November 14, 2025

981
Measurement of Dynamic Force Acted on Water Strider Leg Jumping Upward by the PVDF Film Sensor
07:17

Measurement of Dynamic Force Acted on Water Strider Leg Jumping Upward by the PVDF Film Sensor

Published on: August 3, 2018

6.5K

相关实验视频

Last Updated: Mar 15, 2026

Microparticle Manipulation by Standing Surface Acoustic Waves with Dual-frequency Excitations
06:51

Microparticle Manipulation by Standing Surface Acoustic Waves with Dual-frequency Excitations

Published on: August 21, 2018

7.5K
Investigating the Potential of Singly Curved Thin Piezoelectric Transducers for Energy Harvesting and Structural Health Monitoring
07:02

Investigating the Potential of Singly Curved Thin Piezoelectric Transducers for Energy Harvesting and Structural Health Monitoring

Published on: November 14, 2025

981
Measurement of Dynamic Force Acted on Water Strider Leg Jumping Upward by the PVDF Film Sensor
07:17

Measurement of Dynamic Force Acted on Water Strider Leg Jumping Upward by the PVDF Film Sensor

Published on: August 3, 2018

6.5K

科学领域:

  • 地震学
  • 海洋学
  • 地质学

背景情况:

  • 微震,地震波的振动是由海洋的膨胀产生的.
  • 追踪微震源位置对于理解激发机制至关重要.

研究的目的:

  • 研究来自微地震的地震波组件 (P和S波) 的源位置和能量分区.
  • 了解远处风暴产生的微震的激发机制.

主要方法:

  • 在日本使用地震阵列观察微地震.
  • 分析了来自大西洋暴风雨的P波和S波微震.

主要成果:

  • 观察到的P波和垂直极化S波 (SV波) 与非线性海洋膨胀强迫相一致.
  • 观测到的水平极化S波 (SH波) 无法通过当前的单维地球模型来解释.

结论:

  • 目前的模型充分解释了P和SV波微震,但未能解释SH波.
  • 精确的微震源位置有可能为探索地球内部创造一个新的目录.