stress field वाक्य
उदाहरण वाक्य
मोबाइल
- The interaction between the stress fields of dislocations can impede dislocation motion by repulsive or attractive interactions.
- In substitutional solid solutions, these stress fields are spherically symmetric, meaning they have no shear stress component.
- Dislocation defects also create a stress field.
- A "'stress field "'is a region in a body for which the stress is defined at every point.
- The carbon atoms in the interstitial sites of the lattice creates a stress field that impedes dislocation movement.
- As these interstitial atoms distort the lattice slightly, there will be an associated residual stress field surrounding the interstitial.
- Good examples of this phenomenon are the regions near a coherent precipitate or the stress field around a dislocation.
- The stress fields created by adding solute atoms form the basis of the material strengthening process that occurs in alloys.
- The bonds are clearly stretched around the location of the dislocation and this stretching causes the stress field to form.
- The formation of this field is linked to the rifting of the Andahua valley, as well as local stress fields.
- Lerner-Lam noted, " there is evidence that a large nuclear explosion can change stress fields in the earth's crust ."
- Zobacks'major area of interest is active tectonics, with emphasis on the relationship of the in-situ tectonic stress field to earthquake deformation.
- As dislocations generate repulsive stress fields, each successive dislocation will apply a repulsive force to the dislocation incident with the grain boundary.
- In addition, there is a positive interaction energy between a dislocation and a precipitate that have the same type of stress field.
- Hence, the more dislocations are present in a grain, the greater the stress field felt by a dislocation near a grain boundary:
- When solute and solvent atoms differ in size, local stress fields are created that can attract or repel dislocations in their vicinity.
- The characterization of flow or deformation originating from a simple shear stress field is called shear rheometry ( or shear rheology ).
- The Gulf of Mexico is tectonically passive with low shear strength, but seaward slumping has produced a weak but mappable stress field.
- Intuitively, one can picture the stress fields as the stress created by adding an extra half plane of atoms to a crystal.
- Since both events involved significant north-south shortening, deformation is said to have occurred in response to a similarly oriented in-plane regional stress field.
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