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相关概念视频

Nuclear Binding Energy02:13

Nuclear Binding Energy

The difference between the calculated and experimentally measured masses is known as the mass defect of the atom. In the case of helium-4, the mass defect indicates a “loss” in mass of 4.0331 amu – 4.0026 amu = 0.0305 amu. The loss in mass accompanying the formation of an atom from protons, neutrons, and electrons is due to the conversion of that mass into energy that is evolved as the atom forms. The nuclear binding energy is the energy produced when the atoms’ nucleons are bound together;...
Atomic Nuclei: Nuclear Magnetic Moment00:59

Atomic Nuclei: Nuclear Magnetic Moment

All atomic nuclei are positively charged. When they have a nonzero spin, they behave like rotating charges. As a consequence of their charge and spin, these nuclei generate a magnetic field (B). This, in turn, gives rise to a magnetic moment (μ), which is randomly oriented in the absence of an external magnetic field. When an external magnetic field (B0) is applied, the magnetic moment vectors can align with the field or against it in 2 + 1 orientations. A hydrogen nucleus, which is just a...
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...
Atomic Nuclei: Nuclear Relaxation Processes01:23

Atomic Nuclei: Nuclear Relaxation Processes

In the absence of an external magnetic field, nuclear spin states are degenerate and randomly oriented. When a magnetic field is applied, the spins begin to precess and orient themselves along (lower energy) or against (higher energy) the direction of the field. At equilibrium, a slight excess population of spins exists in the lower energy state. Because the direction of the magnetic field is fixed as the z-axis,  the precessing magnetic moments are randomly oriented around the z-axis. This...
Plastic Deformations of Members with a Single Plane of Symmetry01:21

Plastic Deformations of Members with a Single Plane of Symmetry

When a structural member undergoes plastic deformation due to bending, it is crucial to understand the position of the neutral axis and the stress distribution. This member, characterized by a single plane of symmetry, exhibits a uniform stress distribution, with negative stress above the neutral axis and positive stress below. Notably, the neutral axis does not align with the centroid of the cross-section. This misalignment is typical in cases where the cross-section is not rectangular or...
Dynamic Modulus of Elasticity of Concrete01:16

Dynamic Modulus of Elasticity of Concrete

The dynamic modulus of elasticity assesses how a concrete structure deforms under impact or dynamic loads. It is typically higher than the static modulus of elasticity, measured under slow, steady loading conditions.
The sonic test is a common method to determine the dynamic modulus. In this test, a concrete beam, sized either 6 x 6 x 30 inches or 4 x 4 x 20 inches, is clamped at its center. Vibrations are initiated at one end of the beam by an electromagnetic exciter unit powered by a...

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相关实验视频

Updated: Jul 4, 2026

Sediment Core Extrusion Method at Millimeter Resolution Using a Calibrated, Threaded-rod
06:06

Sediment Core Extrusion Method at Millimeter Resolution Using a Calibrated, Threaded-rod

Published on: August 17, 2016

地震核由M = 7.9Denali,阿拉斯加,地震引起的短暂变形引起的地震核.

J Gomberg1, P Bodin, K Larson

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

Nature
|February 13, 2004
PubMed
概括

2002年德纳利地震引发了北美西部的地震活动,即使在构造压力较低的地区. 这表明动态触发是广泛和不可预测的,发生在临界应力断层上.

科学领域:

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

背景情况:

  • 地震是由压力变化引发的,但这些变化的幅度远小于地震本身释放的压力.
  • 这意味着触发发生在已经具有关键压力的故障上.
  • 升高的孔隙压力,可能来自高温流体,可以减少摩擦应力并促进故障故障.

研究的目的:

  • 为了调查2002年阿拉斯加德纳利地震引发的广泛地震性.
  • 为了确定地震波的动态触发是否被破裂导向性增强.
  • 为了比较德纳利地震引发的触发规模与以前的事件,例如1992年兰德斯地震.

主要方法:

  • 对2002年德纳利地震的地震和高样本GPS记录的分析.
  • 触发的地震性模式与地震断裂导向性的比较.
  • 触发的地震程度与1992年兰德斯地震的地震程度的比较.

主要成果:

  • 2002年德纳利地震在不列颠哥伦比亚省和美国西部引发了广泛的地震性增加.
  • 验证了破裂导向性,以增强特定方向的动态触发.
  • 触发的地震性的规模与1992年兰德斯地震相当.

更多相关视频

Quantitative Hardness Measurement by Instrumented AFM-indentation
08:21

Quantitative Hardness Measurement by Instrumented AFM-indentation

Published on: November 22, 2016

High-pressure, High-temperature Deformation Experiment Using the New Generation Griggs-type Apparatus
12:30

High-pressure, High-temperature Deformation Experiment Using the New Generation Griggs-type Apparatus

Published on: April 3, 2018

相关实验视频

Last Updated: Jul 4, 2026

Sediment Core Extrusion Method at Millimeter Resolution Using a Calibrated, Threaded-rod
06:06

Sediment Core Extrusion Method at Millimeter Resolution Using a Calibrated, Threaded-rod

Published on: August 17, 2016

Quantitative Hardness Measurement by Instrumented AFM-indentation
08:21

Quantitative Hardness Measurement by Instrumented AFM-indentation

Published on: November 22, 2016

High-pressure, High-temperature Deformation Experiment Using the New Generation Griggs-type Apparatus
12:30

High-pressure, High-temperature Deformation Experiment Using the New Generation Griggs-type Apparatus

Published on: April 3, 2018

结论:

  • 大地震的动态触发可以发生在很远的距离和在明显没有构造活动的地区.
  • 即使在环境压力率较低的地区,故障也可能受到严重压力.
  • 动态触发似乎是地震学中无处不在和不可预测的现象.