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相关概念视频

Reflection of Waves01:07

Reflection of Waves

When a wave travels from one medium to another, it gets reflected at the boundary of the second medium. A common example of this is when a person yells at a distance from a cliff and hears the echo of their voice. The sound waves (longitudinal waves) traveling in the air are reflected from the bounding cliff. Similarly, flipping one end of a string whose other end is tied to a wall causes a pulse (transverse wave) to travel through the string, which gets reflected upon reaching the wall. In...
Echo01:06

Echo

The human ear cannot distinguish between two sources of sound if they happen to reach within a specific time interval, typically 0.1 seconds apart. More than this, and they are perceived as separate sources.
Imagine the sound is reflected back to the ears. Assuming that the source is very close to the human, the difference between hearing the two sounds—the emitted sound and the reflected sound—may be more than the minimum time for perceiving distinct sounds. If this is the case, then the...
Travelling Waves01:04

Travelling Waves

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 water;...
Propagation of Waves01:07

Propagation of Waves

When a wave propagates from one medium to another, part of it may get reflected in the first medium, and part of it may get transmitted to the second medium. In such a case, the interface of the two mediums can be considered as a boundary that is neither fixed nor free.
Consider a scenario where a wave propagates from a string of low linear mass density to a string of high linear mass density. In such a case, the reflected wave is out of phase with respect to the incident wave, however the...
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...
Interference and Superposition of Waves01:07

Interference and Superposition of Waves

When two waves of the same nature occur in the same region simultaneously, they result in interference. Interference of waves implies that the net effect of the waves is the sum of the individual waves' effects. However, it does not imply that the individual waves affect the propagation of other waves.
Interference occurs in mechanical waves, such as sound waves, waves on a string, and surface water waves. Mechanical waves correspond to the physical displacement of particles. Hence,...

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相关实验视频

Updated: Jul 11, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
06:04

Simulation of the Planetary Interior Differentiation Processes in the Laboratory

Published on: November 15, 2013

地球外核中的地震波:多重反射

E R Engdahl

    Science (New York, N.Y.)
    |July 19, 1968
    PubMed
    概括

    地球外核中的地震波反射提供了对其结构的新见解. 当前的模型可能需要轻微的速度调整,但核心半径似乎稳定.

    科学领域:

    • 地质物理学 地质物理学
    • 地震学 地震学
    • 地球科学 地球科学 地球科学

    背景情况:

    • 地震波,特别是那些在地球外核中反射的波,为了解地球深层结构提供了宝贵的数据.
    • 以前的地震研究主要集中在核心-地幔边界附近的波浪行为上.

    研究的目的:

    • 分析外核内的地震波反射,以完善其物理性质模型.
    • 调查观察到的地震波到达与当前的地力学模型的一致性.

    主要方法:

    • 对地震波反射的分析,包括外部核心内的多个P波反射 (P P P P).
    • 观察到的波浪到达时间与已建立的地球核心模型的预测进行比较.

    主要成果:

    • 在外核中反射高达四倍的地震波经常被观察到.
    • 观测结果与核心-地幔边界附近的浪潮路径的理论预期一致.
    • 某些观察到的波浪到达需要在当前模型中对外部核心速度进行小调整.
    • 数据不支持接受的核心半径为3473公里的显著变化 (±10公里).

    结论:

    • 这项研究证实了多个地震波反射对于探测外核的实用性.

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    Last Updated: Jul 11, 2026

    Simulation of the Planetary Interior Differentiation Processes in the Laboratory
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    Simulation of the Planetary Interior Differentiation Processes in the Laboratory

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    Dynamic Pore-scale Reservoir-condition Imaging of Reaction in Carbonates Using Synchrotron Fast Tomography
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    Dynamic Pore-scale Reservoir-condition Imaging of Reaction in Carbonates Using Synchrotron Fast Tomography

    Published on: February 21, 2017

    Reservoir Condition Pore-scale Imaging of Multiple Fluid Phases Using X-ray Microtomography
    08:02

    Reservoir Condition Pore-scale Imaging of Multiple Fluid Phases Using X-ray Microtomography

    Published on: February 25, 2015

  • 现有的地震模型可能需要对外核速度进行微调.
  • 地球的外核半径受到分析的地震数据的强烈约束.