Deformation-Mechanism Maps; Creep

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In summary: The first mechanism is collapse at the ideal shear strength. This is the most common type of plasticity and it occurs in metals and ceramics. The second mechanism is low-temperature plasticity by dislocation glide. This is the most common type of plasticity in solids. It can be limited by a lattice resistance, discrete obstacles, phonon or other drags, or influenced by adiabatic heating. The third mechanism is low-temperature plasticity by twinning. This is the most common type of plasticity in crystals. The fourth mechanism is power-law creep by dislocation glide, or glide-plus-climb. This is the least common type of plasticity. The fifth mechanism is diff
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Deformation-Mechanism Maps, The Plasticity and Creep of Metals and Ceramics, by Harold J Frost, Dartmouth College, USA, and Michael F Ashby, Cambridge University, UK.

Creep is a slow plastic flow of a material, and plastic flow is a kinetic process.

In general, the strength of the solid depends on both strain and strain-rate, and on temperature. It is determined by the kinetics of the processes occurring on the atomic scale: the glide-motion of dislocation lines; their coupled glide and climb; the diffusive flow of individual atoms; the relative displacement of grains by grain boundary sliding (involving diffusion and defect-motion in the boundaries); mechanical twinning (by the motion of twinning dislocations) and so forth. These are the underlying atomistic processes which cause flow. But it is more convenient to describe polycrystal plasticity in terms of the mechanisms to which the atomistic processes contribute. We therefore consider the following deformation mechanisms, divided into five groups.

Collapse at the ideal strength —(flow when the ideal shear strength is exceeded).
Low-temperature plasticity by dislocation glide—(a) limited by a lattice resistance (or Peierls' stress); (b) limited by discrete obstacles; (c) limited by phonon or other drags; and (d) influenced by adiabatic heating.
Low-temperature plasticity by twinning.
Power-law creep by dislocation glide, or glide-plus-climb —(a) limited by glide processes; (b) limited by lattice-diffusion controlled climb (“high-temperature creep”); (c) limited by core*diffusion controlled climb (“low-temperature creep”); (d) power-law breakdown, (the transition from climb-plus-glide to glide alone); (e) Harper-Dorn creep; (f) creep accompanied by dynamic recrystallization.
Diffusional Flow—(a) limited by lattice diffusion (“Nabarro-Herring creep”); (b) limited by grain boundary diffusion (“Coble creep”); and (c) interface-reaction controlled diffusional flow.

http://engineering.dartmouth.edu/defmech/

I'll elaborate later, but others are certainly welcome and encouraged to contribute.
 
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One of my thesis committee members, an outstanding metallurgist, taught me: "There is no such thing as elasticity, only negligible plasticity." Creep occurs in all materials at all temperatures; nothing is immune. Of course, the deformation is generally undetectable at less than a considerable fraction -- perhaps one-third or one-half -- of the absolute melting temperature.
 

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The text does make such a point - "Although it is often convenient to think of a polycrystalline solid as having a well defined yield strength, below which it does not flow and above which flow is rapid, this is true only at absolute zero."
 

FAQ: Deformation-Mechanism Maps; Creep

What is a deformation-mechanism map?

A deformation-mechanism map is a graphical representation of the dominant deformation mechanisms in a material at different temperature and stress conditions. It helps scientists and engineers understand how a material will deform and fail under different loading conditions.

How are deformation-mechanism maps created?

Deformation-mechanism maps are created using experimental data from various tests, such as creep tests and stress-strain tests. The data is then plotted on a graph with temperature and stress as the independent variables and the dominant deformation mechanism as the dependent variable. The resulting map is often divided into different regions representing different deformation mechanisms.

What is creep and why is it important in deformation-mechanism maps?

Creep is the time-dependent deformation of a material under a constant load. It is an important factor in deformation-mechanism maps because it can significantly affect the mechanical properties and failure of a material. Creep data is often used to determine the boundaries between different deformation mechanisms on the map.

How can deformation-mechanism maps be useful in material design?

Deformation-mechanism maps can be useful in material design by allowing scientists and engineers to predict the behavior of a material under different conditions. This information can help in selecting the appropriate material for a specific application and designing components that can withstand the expected loading conditions.

What are the limitations of deformation-mechanism maps?

Deformation-mechanism maps have some limitations, such as being only applicable to specific materials and not accounting for microstructural changes that may occur during deformation. Additionally, the data used to create the maps may not accurately represent all possible loading conditions, leading to some degree of uncertainty in the predictions made using the map.

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