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相关概念视频

Shearing Stress01:18

Shearing Stress

2.5K
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.
2.5K
Stress-Strain Diagram - Brittle Materials01:24

Stress-Strain Diagram - Brittle Materials

4.5K
Brittle materials, including glass, cast iron, and stone, exhibit unique characteristics. They fracture without considerable change in their elongation rate, indicating that their breaking and ultimate strength are equivalent. Such materials also show lower strain levels at the point of rupture. The failure in brittle materials predominantly results from normal stresses, as evidenced by the rupture created along a surface perpendicular to the applied load. These materials do not display...
4.5K
Yield Criteria for Ductile Materials under Plane Stress01:25

Yield Criteria for Ductile Materials under Plane Stress

836
In designing structural elements and machine parts using ductile materials, it is crucial to ensure that these components withstand applied stresses without yielding. Yielding is initially determined through a tensile test, which evaluates the material's response to uniaxial stress. However, tensile stress is insufficient when components face biaxial or plane stress conditions This condition requires advanced criteria to predict failure.
The Maximum Shearing Stress Criterion, also known as...
836
Elastic Strain Energy for Shearing Stresses01:20

Elastic Strain Energy for Shearing Stresses

668
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...
668
Tensile Strength Considerations of Concrete01:16

Tensile Strength Considerations of Concrete

1.7K
Considering the tensile strength of concrete involves recognizing that the theoretical strength of cement paste can be up to a thousand times higher than what is observed in practical applications. This significant discrepancy is largely attributed to the presence of microscopic cracks within the concrete. These cracks tend to amplify stress at their tips when a load is applied, a phenomenon explained by Griffith's theory of brittle fracture.
The dimensions and shape of a concrete specimen...
1.7K
Behavior of Concrete Under Compressive Load01:23

Behavior of Concrete Under Compressive Load

949
Concrete exhibits specific behaviors under different compressive loads. Understanding this is crucial for understanding its structural integrity. When concrete undergoes uniaxial compression, it tends to develop cracks that run parallel to the direction of the force. These parallel cracks stem from localized tensile stresses that occur perpendicular to the compression direction. Additionally, angled cracks may appear due to the formation of shear planes.
As the concrete specimen fractures under...
949

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相关实验视频

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A Method for Studying the Temperature Dependence of Dynamic Fracture and Fragmentation
09:12

A Method for Studying the Temperature Dependence of Dynamic Fracture and Fragmentation

Published on: June 28, 2015

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通过拉伸裂纹相互作用的三维脆性剪切裂纹.

David Healy1, Richard R Jones, Robert E Holdsworth

  • 1Rock Deformation Laboratory, Department of Earth and Ocean Sciences, University of Liverpool, Liverpool L69 3GP, UK. dhealy@liverpool.ac.uk

Nature
|January 7, 2006
PubMed
概括

研究人员开发了一种新的3D模型,解释了易碎岩石中的多模式断层模式. 这种微裂相互作用模型提高了对岩石破裂的理解,这对于地震地震学和岩石质量稳定性至关重要.

科学领域:

  • 地质物理学 地质物理学
  • 岩石机械学 岩石机械学
  • 材料科学 材料科学 材料科学

背景情况:

  • 脆性岩石的断层源于相互作用的拉力微裂.
  • 像库伦-莫尔这样的现有模型无法解释复杂的3D多模式故障模式.
  • 微裂纹几何和应力场决定了剪切断裂的方向.

研究的目的:

  • 开发一个3D模型,解释易碎岩石中的多模式断层模式.
  • 为了解释岩石破裂中拉力微裂的相互作用.
  • 为了更好地了解脆性剪切故障机制.

主要方法:

  • 利用基于Eshelby的解决方案的3D微裂纹交互模型.
  • 在三维中分析了拉力微裂周围的弹性应力场.
  • 将3D模型与之前的2D近似进行对比.

主要成果:

  • 3D模型成功地解释了多模式故障模式的形成.
  • 微裂纹相互作用产生斜向向远程主应力的剪切平面.
  • 预测的剪切断裂与压缩轴最多倾斜26度.

结论:

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  • 三维微裂纹相互作用模型为观察到的断裂模式提供了强有力的解释.
  • 这项研究有助于我们更好地理解地质材料中脆性剪切失效的现象.
  • 这些发现对地震地震学,岩石质量的稳定性和流体迁移有重大影响.