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相关概念视频

The Soil Ecosystem02:23

The Soil Ecosystem

Plants obtain inorganic minerals and water from the soil, which acts as a natural medium for land plants. The composition and quality of soil depend not only on the chemical constituents but also on the presence of living organisms. In general, soils contain three major components:
Tidal Forces01:06

Tidal Forces

The origin of Earth's ocean tides has been a subject of continuous investigation for over 2000 years. However, the work of Newton is considered to be the beginning of the proper understanding of the phenomenon. Ocean tides are the result of gravitational tidal forces. These same tidal forces are present in any astronomical body; they are responsible for the internal heat that creates the volcanic activity on Io, one of Jupiter's moons, and the breakup of stars that get too close to black holes.
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;...
Kinetic and Potential Energy of a Wave01:10

Kinetic and Potential Energy of a Wave

All forms of waves carry energy; this is directly visualized in nature. For instance, the waves of earthquakes are so intense that they can shake huge concrete buildings, causing them to fall. Loud sounds can damage nerve cells in the inner ear, causing permanent hearing loss. The waves of the oceans can erode beaches. 
In mechanical waves, the amount of energy is related to their amplitude and frequency. In the context of the above examples, large-amplitude earthquakes produce large ground...
Modes of Standing Waves - I01:03

Modes of Standing Waves - I

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 phenomenon...
Generating Electromagnetic Radiations01:10

Generating Electromagnetic Radiations

The German physicist Heinrich Hertz (1857–1894) was the first to generate and detect certain types of electromagnetic waves in the laboratory. Starting in 1887, he performed a series of experiments that confirmed the existence of electromagnetic waves and verified that they travel at the speed of light. Hertz used an alternating-current RLC (resistor-inductor-capacitor) circuit that resonated at a known frequency and connected it to a loop of wire. High voltages induced across the gap in the...

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相关实验视频

Updated: Jul 11, 2026

Blast Quantification Using Hopkinson Pressure Bars
09:41

Blast Quantification Using Hopkinson Pressure Bars

Published on: July 5, 2016

地震是由地震波引发的,其次是Landers和Hector矿山地震.

J Gomberg1, P A Reasenberg, P Bodin

  • 1US Geological Survey, Center for Earthquake Research and Information, 3876 Central Avenue Suite 2, Memphis, Tennessee 38152-3050, USA. gomberg@usgs.gov

Nature
|May 25, 2001
PubMed
概括

大地震产生的暂时的地震波可以引发余震. 动态应力变化超过静态应力变化,在这种地震触发现象中起着关键作用,特别是在更远的距离上.

科学领域:

  • 地震地震学 地震学
  • 地质物理学 地质物理学
  • 构造学 构造学 构造学 构造学

背景情况:

  • 1992年的兰德斯地震和1999年的赫克托矿山地震为研究地震触发提供了独特的机会.
  • 以前的研究表明,地震波的动态变形可以增加地震率.

研究的目的:

  • 量化Landers和Hector矿山地震后地震率变化的空间和时间模式.
  • 研究动态和静态应力变化在地震触发中的作用.
  • 确定动态触发值及其与当地条件的关系.

主要方法:

  • 对响应Landers和Hector矿山地震的地震率变化的分析.
  • 观察到的地震性模式与地震波传播和应力变化模型的比较.
  • 测量顶峰地震速度以推断动态触发值.

主要成果:

  • 在Landers的北部和Hector Mine的南部观察到地震率的增加,与破裂的方向性一致.
  • 动态和静态应力变化都有助于触发,动态应力在更远的距离上占主导地位.
  • 据估计,动态触发值在十分之一到几MPa之间,明显高于静态值.
  • 在动态变形减缓后,在一些地点观察到延迟触发.

更多相关视频

Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
07:58

Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt

Published on: August 7, 2017

Experimental Methods of Dust Charging and Mobilization on Surfaces with Exposure to Ultraviolet Radiation or Plasmas
07:54

Experimental Methods of Dust Charging and Mobilization on Surfaces with Exposure to Ultraviolet Radiation or Plasmas

Published on: April 3, 2018

相关实验视频

Last Updated: Jul 11, 2026

Blast Quantification Using Hopkinson Pressure Bars
09:41

Blast Quantification Using Hopkinson Pressure Bars

Published on: July 5, 2016

Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
07:58

Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt

Published on: August 7, 2017

Experimental Methods of Dust Charging and Mobilization on Surfaces with Exposure to Ultraviolet Radiation or Plasmas
07:54

Experimental Methods of Dust Charging and Mobilization on Surfaces with Exposure to Ultraviolet Radiation or Plasmas

Published on: April 3, 2018

结论:

  • 作为地震波辐射的动态变形是触发地震性的重要因素.
  • 断裂导向性影响动态应力和随后的地震性的空间分布.
  • 这些发现支持地震触发过程中的液化或循环疲劳等物理机制.