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  2. Creep (deformation) - Wikipedia

    en.wikipedia.org/wiki/Creep_(deformation)

    In materials science, creep (sometimes called cold flow) is the tendency of a solid material to undergo slow deformation while subject to persistent mechanical stresses. It can occur as a result of long-term exposure to high levels of stress that are still below the yield strength of the material. Creep is more severe in materials that are ...

  3. Viscoelasticity - Wikipedia

    en.wikipedia.org/wiki/Viscoelasticity

    In materials science and continuum mechanics, viscoelasticity is the property of materials that exhibit both viscous and elastic characteristics when undergoing deformation. Viscous materials, like water, resist both shear flow and strain linearly with time when a stress is applied.

  4. Diffusion creep - Wikipedia

    en.wikipedia.org/wiki/Diffusion_creep

    Diffusion creep is caused by the migration of crystalline defects through the lattice of a crystal such that when a crystal is subjected to a greater degree of compression in one direction relative to another, defects migrate to the crystal faces along the direction of compression, causing a net mass transfer that shortens the crystal in the ...

  5. Grain boundary sliding - Wikipedia

    en.wikipedia.org/wiki/Grain_boundary_sliding

    Grain boundary sliding (GBS) is a material deformation mechanism where grains slide against each other. This occurs in polycrystalline material under external stress at high homologous temperature (above ~0.4 [1]) and low strain rate and is intertwined with creep.

  6. Downhill creep - Wikipedia

    en.wikipedia.org/wiki/Downhill_creep

    Downhill creep, also known as soil creep or commonly just creep, is a type of creep characterized by the slow, downward progression of rock and soil down a low grade slope; it can also refer to slow deformation of such materials as a result of prolonged pressure and stress.

  7. Coble creep - Wikipedia

    en.wikipedia.org/wiki/Coble_creep

    In materials science, Coble creep, a form of diffusion creep, is a mechanism for deformation of crystalline solids. Contrasted with other diffusional creep mechanisms, Coble creep is similar to Nabarro–Herring creep in that it is dominant at lower stress levels and higher temperatures than creep mechanisms utilizing dislocation glide. [ 1 ]

  8. Stress relaxation - Wikipedia

    en.wikipedia.org/wiki/Stress_relaxation

    In materials science, stress relaxation is the observed decrease in stress in response to strain generated in the structure. This is primarily due to keeping the structure in a strained condition for some finite interval of time hence causing some amount of plastic strain.

  9. Dislocation creep - Wikipedia

    en.wikipedia.org/wiki/Dislocation_creep

    This expression is derived from a model from which plastic strain does not devolve from atomic diffusion. [2] The creep rate is defined by the intrinsic activation energy and the ratio of stress-assisted energy to thermal energy (). The creep rate increases as this ratio increases, or as stress-assisted energy increases more than thermal energy.