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Related Concept Videos

Shear Diagram01:27

Shear Diagram

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In the study of beam mechanics, shear diagrams play a crucial role in understanding the distribution of shear forces along the length of a beam. Consider a beam AB that is supported at both ends and subjected to perpendicular loads.
First, a free-body diagram of the beam is drawn, representing all the external forces and internal reactions acting on the beam. One can calculate the reaction forces at each support by employing the equilibrium equations of force and moment. The vertical component...
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Shearing Stress01:19

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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.
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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 the...
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Pure cultures, defined as the growth of a single microorganism species isolated from mixed populations, are fundamental tools in microbiological research and practical applications. These cultures ensure genetic and physiological uniformity, allowing researchers to study microbial traits under controlled conditions.Isolation and Maintenance of Pure CulturesObtaining a pure culture involves isolating a single microbial type from a mixed sample through techniques such as serial dilutions, streak...
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Visualization of Failure and the Associated Grain-Scale Mechanical Behavior of Granular Soils under Shear using Synchrotron X-Ray Micro-Tomography
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Visualization of Failure and the Associated Grain-Scale Mechanical Behavior of Granular Soils under Shear using Synchrotron X-Ray Micro-Tomography

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Patterning of a cohesionless granular layer under pure shear.

Héctor Alarcón1,2, Jean-Christophe Géminard3, Francisco Melo1

  • 1Departamento de Física, Universidad de Santiago de Chile, Av. Ecuador 3493, Casilla 307, Correo 2, Santiago, Chile.

Physical Review. E
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Summary

Granular materials exhibit complex deformation patterns under shear. For noncohesive materials, this instability arises from reduced friction, unlike cohesive materials where it

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Area of Science:

  • Complex Systems
  • Pattern Formation
  • Granular Mechanics
  • Rheology

Background:

  • Previous studies on cohesive granular materials under stretching revealed fracture patterns.
  • Instability in cohesive materials is attributed to the rupture of capillary bridges bonding grains.
  • Noncohesive granular materials lack capillary bridges, necessitating alternative explanations for instability.

Purpose of the Study:

  • To investigate the response of thin layers of noncohesive granular material to pure shear at the base.
  • To identify the underlying mechanisms causing deformation inhomogeneity in noncohesive granular materials.
  • To contrast the observed patterns with those in cohesive granular materials.

Main Methods:

  • Experimental investigation of granular material response to imposed pure shear.
  • Utilized image-correlation technique to reveal surface deformation patterns.
  • Focused on noncohesive granular materials.

Main Results:

  • Observed inhomogeneous deformation in thin layers of noncohesive granular material.
  • Revealed a novel smooth pattern characterized by periodic modulation of shear deformation on the free surface.
  • Demonstrated that instability in noncohesive materials results from a decrease in friction during shearing.

Conclusions:

  • The deformation of noncohesive granular materials under shear is inherently inhomogeneous.
  • A new pattern of surface deformation modulation has been identified.
  • Reduced friction during shearing is the primary cause of instability in noncohesive granular materials.