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| '''Diffusion creep''' refers to the [[Deformation (mechanics)|deformation]] of [[crystalline]] solids by the [[diffusion]] of [[Vacancy defect|vacancies]] through their [[crystal lattice]].<ref>Passchier & Trouw 1998; p. 257</ref> Diffusion creep results in [[plastic deformation]] rather than [[brittle failure]] of the material.
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| Diffusion creep is more sensitive to [[temperature]] than other [[deformation mechanism]]s. It usually takes place at high [[homologous temperature]]s (i.e. within about a tenth of its absolute [[melting]] temperature). Diffusion creep is caused by the migration of [[Crystallographic defect|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 direction of maximum compression. The migration of defects is in part due to vacancies, whose migration is equal to a net mass transport in the opposite direction.
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| ==Principle==
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| Crystalline materials are never perfect on a microscale. Some sites of atoms in the crystal lattice can be occupied by [[point defect]]s, such as "alien" particles or vacancies. Vacancies can actually be thought of as chemical species themselves (or part of a compound species/component) that may then be treated using heterogeneous [[Gibbs' phase rule|phase equilibria]]. The number of vacancies may also be influenced by the number of chemical impurities in the crystal lattice, if such impurities require the formation of vacancies to exist in the lattice.
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| A vacancy can move through the crystal structure when the neighbouring particle "jumps" in the vacancy, so that the vacancy moves in effect one site in the crystal lattice. [[Chemical bond]]s need to be broken and new bonds have to be formed during the process,<ref>Twiss & Moores 2000, p. 391</ref> therefore a certain [[activation energy]] is needed. Moving a vacancy through a crystal becomes therefore easier when the [[temperature]] is higher.
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| The most stable state will be when all vacancies are evenly spread through the crystal. This principle follows from [[Fick's law]]:
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| : <math> J_x = -D_x \frac{\Delta C}{\Delta x} </math>
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| In which ''J<sub>x</sub>'' stands for the [[flux]] ("flow") of vacancies in direction ''x''; ''D''<sub>''x''</sub> is a [[Constant (mathematics)|constant]] for the material in that direction and <math>{\Delta C}/{\Delta x}</math> is the difference in concentration of vacancies in that direction. The law is valid for all principal directions in (''x'', ''y'', ''z'')-space, so the ''x'' in the formula can be exchanged for ''y'' or ''z''. The result will be that they will become evenly distributed over the crystal, which will result in the highest [[Entropy of mixing|mixing entropy]].
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| When a [[mechanical stress]] is applied to the crystal, new vacancies will be created at the sides perpendicular to the direction of the lowest [[principal stress]]. The vacancies will start moving in the direction of crystal planes perpendicular to the maximal stress.<ref>Twiss & Moores 2000; p. 390-391</ref> Current theory holds that the [[Elasticity (physics)|elastic]] [[Strain (materials science)|strain]] in the neighborhood of a defect is smaller toward the axis of greatest differential compression, creating a defect chemical [[potential gradient]] (depending upon lattice strain) within the crystal that leads to net accumulation of defects at the faces of maximum compression by diffusion. A flow of vacancies is the same as a flow of particles in the opposite direction. This means a crystalline material can deform under a [[differential stress]], by the flow of vacancies.
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| Highly mobile chemical components substituting for other species in the lattice can also cause a net differential mass transfer (i.e. segregation) of chemical species inside the crystal itself, often promoting shortening of the [[rheology|rheologically]] more difficult substance and enhancing deformation.
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| ==Types of diffusion creep==
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| Diffusion of vacancies through a crystal can happen in a number of ways. When vacancies move through the crystal (in the material sciences often called a "grain"), this is called ''[[Nabarro-Herring creep]]''. Another way in which vacancies can move is along the [[grain boundary|grain boundaries]], a mechanism called ''[[Coble creep]]''.
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| When a crystal deforms by diffusion creep to accommodate space problems from simultaneous [[grain boundary sliding]] (the movement of whole grains along grain boundaries) this is called ''[[granular flow|granular or superplastic flow]]''.<ref>Twiss & Moores 2000, p. 394</ref> Diffusion creep can also be simultaneous with [[pressure solution]]. Pressure solution is, like Coble creep, a mechanism in which material moves along grain boundaries. While in Coble creep the particles move by "dry" diffusion, in pressure solution they move in [[solution (chemistry)|solution]].
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| ==Flow laws==
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| Each plastic deformation of a material can be described by a formula in which the [[strain rate]] (<math>\dot{\epsilon}</math>) depends on the differential stress (''σ'' or ''σ''<sub>D</sub>), the grain size (''d'') and an activation value in the form of an [[Arrhenius equation]]:<ref>Passchier & Trouw 1998; p. 54</ref>
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| <math>\!\dot{\epsilon} = Ae^\frac{-Q}{RT} \frac{\sigma^n}{d^m}</math>
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| In which ''A'' is the constant of diffusion, ''Q'' the activation energy of the mechanism, ''R'' the [[gas constant]] and ''T'' the [[absolute temperature]] (in [[Kelvin (unit)|kelvins]]). The exponents ''n'' and ''m'' are values for the sensitivity of the flow to stress and grain size respectively. The values of ''A'', ''Q'', ''n'' and ''m'' are different for each deformation mechanism. For diffusion creep, the value of ''n'' is usually around 1. The value for ''m'' can vary between 2 (Nabarro-Herring creep) and 3 (Coble creep). That means Coble creep is more sensitive to grain size of a material: materials with larger grains can deform less easily by Coble creep than materials with small grains.
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| ==Traces of diffusion creep==
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| It is difficult to find clear microscale evidence for diffusion creep in a crystalline material, since little structures have been identified as definite proof. A material that was deformed by diffusion creep can have flattened grains (grains with a so called [[shape-preferred orientation]] or SPO). Equidimensional grains with no [[lattice-preferred orientation]] (or LPO) can be an indication for superplastic flow.<ref>Passchier & Trouw 1998; p. 42</ref> In materials that were deformed under very high temperatures, lobate grain boundaries may be taken as evidence for diffusion creep.<ref>Gower & Simpson 1992</ref>
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| Diffusion creep is a mechanism by which the volume of the crystals can increase. Larger grain sizes can be a sign that diffusion creep was more effective in a crystalline material.
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| ==See also==
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| *[[creep (deformation)]]
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| *[[deformation (engineering)]]
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| *[[diffusion]]
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| *[[dislocation creep]]
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| *[[material sciences]]
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| ==References==
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| {{reflist|30em}}
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| ===Literature===
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| *Gower, R.J.W. & Simpson, C.; 1992: ''Phase boundary mobility in naturally deformed, high-grade quartzofeldspatic rocks: evidence for diffusion creep'', Journal of Structural Geology '''14''', p. 301-314.
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| *Passchier, C.W. & Trouw, R.A.J., 1998: ''Microtectonics'', Springer, ISBN 3-540-58713-6
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| *Twiss, R.J. & Moores, E.M., 2000 (6th edition): ''Structural Geology'', W.H. Freeman & co, ISBN 0-7167-2252-6
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| [[Category:Materials degradation]]
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