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相关概念视频

True Stress and True Strain01:28

True Stress and True Strain

281
Engineering stress is calculated as the load divided by the original, undeformed cross-sectional area. It approximates a material under load. This approximation is especially relevant post-yield in ductile materials. Though engineering stress-strain diagrams are often used for their convenience and accessibility, they can sometimes fall short in accuracy, particularly when dealing with large strain values.
In contrast, true stress offers a more precise portrayal. It is computed by dividing the...
281
Stress-Strain Diagram - Ductile Materials01:24

Stress-Strain Diagram - Ductile Materials

653
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...
653
Stress-Strain Diagram - Brittle Materials01:24

Stress-Strain Diagram - Brittle Materials

2.2K
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...
2.2K
Three-Dimensional Analysis of Strain01:29

Three-Dimensional Analysis of Strain

209
Three-dimensional strain analysis is crucial for understanding how materials deform under stress, particularly in elastic, homogeneous materials. This method employs principal stress axes to simplify complex stress states into more understandable forms. Subjected to stress, a small cubic element within a material either expands or contracts along these axes, transforming into a rectangular parallelepiped. This transformation effectively illustrates the material's deformation. The principal...
209
Shearing Strain01:20

Shearing Strain

239
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...
239
Relation between Poisson's ratio, Modulus of Elasticity and Modulus of Rigidity01:15

Relation between Poisson's ratio, Modulus of Elasticity and Modulus of Rigidity

256
Deformation occurs in axial and transverse directions when an axial load is applied to a slender bar. This deformation impacts the cubic element within the bar, transforming it into either a rectangular parallelepiped or a rhombus, contingent on its orientation. This transformation process induces shearing strain. Axial loading elicits both shearing and normal strains. Applying an axial load instigates equal normal and shearing stresses on elements oriented at a 45° angle to the load axis.
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Full-field Strain Measurements for Microstructurally Small Fatigue Crack Propagation Using Digital Image Correlation Method
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在状岩石中预失败应变定位:实验室和数值方法的比较研究.

Patrick Bianchi1, Paul Antony Selvadurai1, Luca Dal Zilio2,3,4

  • 1Swiss Seismological Service, ETH Zurich, Zurich, Switzerland.

Rock mechanics and rock engineering
|August 22, 2024
PubMed
概括

研究人员使用实验室测试和计算机模型研究了砂岩中的地震前体过程. 他们观察了应变局部化和声学辐射,揭示了岩石破裂前的不同变形阶段.

关键词:
声学排放 声学排放 是一种基于连续性的数值建模.使用光纤进行分布式应变传感.准备过程 准备过程菌株局部化 菌株局部化

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科学领域:

  • 地质物理学 地质物理学
  • 岩石机械学 岩石机械学
  • 计算科学 计算科学

背景情况:

  • 了解地震准备过程对于地震预测至关重要.
  • 变形局部化和声学排放是岩石破裂的关键指标.
  • 之前的研究往往缺乏综合实验室和数值方法.

研究的目的:

  • 为了研究 (a) 岩石变形过程中的地震准备过程.
  • 为了将实验室观察结果与数值建模结果相关联.
  • 阐明砂岩变形局部化和失效的物理.

主要方法:

  • 结合实验室三轴故障测试与基于物理的计算模型.
  • 利用分布式应变传感 (DSS) 和声辐射 (AE) 技术.
  • 量化应变局部化和地震活动.

主要成果:

  • 确定了三个不同的准备过程阶段:消散前线,P波速度下降,并带形成.
  • 观察到扩张性叶片导致应变局部化和加速变形.
  • 与实验应变速率测量和地震性相关的模拟变形.

结论:

  • 综合实验室和数值方法为 (a) 地震准备过程提供了全面的视图.
  • 该研究阐明了岩石破裂之前的变形局部化的时空演变.
  • 这些发现增强了我们对岩石质量在压力下行为的理解.