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相关概念视频

Shearing Stress01:19

Shearing Stress

524
Shearing stress, denoted by the Greek letter tau (τ), is stress caused by forces acting transversely on an object. These forces create internal ones within the entity in the plane where the external forces are applied. The resultant of these internal forces is the shear in the section.
The average shearing stress can be calculated by dividing the shear by the area of the cross-section.
524
Elastic Strain Energy for Shearing Stresses01:20

Elastic Strain Energy for Shearing Stresses

165
As discussed in previous lessons, strain energy in a material is the energy stored when it is elastically deformed, a concept crucial in materials science and mechanical engineering. This energy results from the internal work done against the cohesive forces within the material. When a material undergoes shearing stress and corresponding shearing strain, the strain energy density, which is the energy stored per unit volume, is calculated. Within the elastic limit, where the stress is...
165
Shearing Strain01:20

Shearing Strain

229
The shearing strain represents a cubic element's angular change when subjected to shearing stress. This type of stress can transform a cube into an oblique parallelepiped without influencing normal strains. The cubic element experiences a significant transformation when exposed solely to shearing stress. Its shape alters from a perfect cube into a rhomboid, clearly demonstrating the effect of shearing strain. The degree of this strain is considered positive if it reduces the angle between...
229
Relation Between the Distributed Load and Shear01:23

Relation Between the Distributed Load and Shear

607
Understanding the relationship between the distributed load and shear force in structural analysis is crucial for analyzing beams subjected to various loading conditions. Consider the case of a beam experiencing a distributed load, two concentrated loads, and a couple moment.
607
Stress: General Loading Conditions01:15

Stress: General Loading Conditions

301
To grasp the intricacy of real-world conditions where multiple loads are applied simultaneously to a structure, one might visualize a section passing through a specific point within a body, aligned parallel to the xy plane. This section is subjected to various forces, including original loads, normal forces, and shearing forces.
The shearing force, possessing potential directionality within the plane of the section, is simplified into two component forces running parallel to the x and y axes....
301
Stress-Strain Diagram - Ductile Materials01:24

Stress-Strain Diagram - Ductile Materials

638
The stress-strain relationship in ductile materials such as structural steel or aluminium is intricate and progresses through several stages. When a specimen is loaded, it initially exhibits a linear length increase, depicted by a steep straight line on the stress-strain diagram. It indicates the material is elastically deforming and will return to its original shape once unloaded. However, when a critical stress value is reached, plastic deformation begins. This stage sees substantial...
638

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相关实验视频

Updated: Jun 9, 2025

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
06:55

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling

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在俯冲启动过程中,快速切割区在俯冲启动期间变弱.

Yida Li1, Michael Gurnis1

  • 1Division of Geological and Planetary Sciences, Seismological Laboratory, California Institute of Technology, Pasadena, CA 91125.

Proceedings of the National Academy of Sciences of the United States of America
|October 25, 2024
PubMed
概括

由于快速应变减弱,引启动迅速发生,正如在Puysegur的例子中观察到的那样. 这一发现为早期地球构造学和板块运动的开始提供了洞察力.

科学领域:

  • 地质物理学 地质物理学
  • 构造学 构造学 构造学 构造学
  • 地球科学 地球科学 地球科学

背景情况:

  • 俯冲区对于板块构造学至关重要,通过板块拉动和弱大的巨型冲击驱动板块运动.
  • 俯冲启动与板块拉力积累和板块边界弱点有关,显著改变了地幔对流.
  • 潜伏启动期间的短暂性质和强烈活动掩盖了关键证据,使其难以研究.

研究的目的:

  • 通过分析受良好的约束的Puysegur示例来克服研究降温启动的局限性.
  • 通过先进的计算和观察方法,研究俯冲启动的机制和特征.

主要方法:

  • 进行了时间依赖的三维热力学计算.
  • 与新的地质物理和地质数据 (地形学,地层学,地震性) 进行定量比较.

主要成果:

  • 证明了潜伏启动与快速应变减弱一起发展,其特点是小位移 (48公里).
  • 确定了快速减弱的潜在物理机制,包括粒径减小和流体加压.
  • 普伊塞格尔的例子可以作为一个非常受约束的实例研究,用于降温启动.

结论:

  • 在Puysegur观测到的快速压力减弱提供了对早期地球潜水带形成的见解.
关键词:
新西兰新西兰新西兰新西兰地力学地力学是什么板块构造学板块构造学是什么意思潜入的潜入方式

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  • 了解俯冲开始是理解板块构造学开始和演变的关键.
  • 这些发现对了解早期地球和潜在的其他行星天体上的构造过程有意义.