2.2.2 Local and Global Equilibrium

Global thermal equilibrium at arbitrary temperatures, i.e. the absolute minimum of the free enthalpy, can only be achieved if there are mechanisms for the generation and annihilation of point defects.
There must be sources and sinks for vacancies and (intrinsic) interstitials that operate with small activation energies - otherwise it will take a long time before global equilibrium will be achieved.
At this point it is essential to appreciate that an ideal perfect (= infinitely large) crystal has no sources and sinks - it can never be in thermal equilibrium. An atom, for example, cannot simply disappear leaving a vacancy behind and then miraculously appear at the surface, as we assumed in equilibrium thermodynamics, where it does not matter how a state is reached.
On the other hand, infinitely large perfect crystals do not exist - but semiconductor-grade dislocation-free single Si crystals with diameters of 300 mm and beyond, and lengths of up to 1 m are coming reasonably close. They form a special case as far as point defects are concerned.
Otherwise we need other defects - grain boundaries, dislocations, precipitates and so on as sources and sinks for point defects. And that is what we almost always have in regular metals or ceramics.
How a grain boundary can act as source or sink for vacancies is schematically shown in the pictures below.
It is clear form these drawings that the activation energy (which is not the formation energy of a vacancy!!) needed to emit (not to form from scratch!) a vacancy from a grain boundary is small.
 
Grain boundary as vacancy source Grain boundary as vacancy sink
Grain boundary absorbs 1 vacancy, i.e. acts as sink for one more jump of the proper atom. Grain boundary emits 3 vacancies, i.e. acts as source for one more jump of the 3 proper atoms.
The red arrows indicate the jumps of individual atoms. The flux of the vacancies is always opposite to the flux of diffusing atoms.
 
We thus may expect that at sufficiently high temperatures (meaning temperatures large enough to allow diffusion), we will be able to establish global point defect equilibrium in a real (= non-ideal) crystal, but not really global crystal equilibrium, because a crystal with dislocations and grain boundaries is never at equilibrium.
Sources and sinks are a thus a necessary, but not a sufficient ingredient for point defect equilibrium. We also must require that the point defects are able to move, there must be some diffusion - or you must resign yourself to waiting for a long time.
At low temperatures, when all diffusion effectively stops, nothing goes anymore. Equilibrium is unreachable. For many practical cases however, this is of no consequence. At temperatures where diffusion gets sluggish, the equilibrium concentration ceq is so low, that you cannot measure it. For all practical purposes it surely doesn't matter if you really achieve, for example, ceq = 10–14, or if you have non-equilibrium with the actual concentration c a thousand times larger than ceq (i.e. c = 10–11). For all practical purposes we have simply c = 0.
At high temperatures, when diffusion is fast, point defect equilibrium will be established very quickly in all real crystals with enough sources and sinks.
The intermediate temperatures thus are of interest. The mobility is not high enough to allow many point defects to reach convenient sinks, but not yet too small to find other point defects.
In other words, the average diffusion length or mean distance covered by a randomly diffusing point defect in the time interval considered, is smaller than the average distance between sinks, but larger than the average distance between point defects.
Global point defect equilibrium as the best solution is thus unattainable at medium temperatures, but local equilibrium is now the second best choice and far preferable to a huge supersaturation of single point defects slowly moving through the crystal in search of sinks.
Local equilibrium then simply refers to the state with the smallest free enthalpy taking into account the restraints of the system. The most simple restraint is that the total number of vacancies in vacancy clusters of all sizes (from single vacancy to large "voids") is constant. This acknowledges that vacancies cannot be annihilated at sinks under these conditions, but still are able to cluster.
Let us illustrate this with a relevant example. Consider vacancies in a metal crystal that is cooled down after it has been formed by casting.
As the temperature decreases, global equilibrium demands that the vacancy concentration decreases exponentially. As long as the vacancies are very mobile, this is possible by annihilation at internal sinks.
However, at somewhat lower temperatures, the vacancies are less mobile and have not enough time to reach sinks like grain boundaries, but can still cover distances much larger than their average separation. This means that divacancies, trivacancies and so on can still form - up to large clusters of vacancies, either in the shape of a small hole or void, or, in a two-dimensional form, as small dislocation loops. Until they become completely immobile, the vacancies will be able to cover a distance given by the diffusion length L (which depends, of course, on how quickly we cool down).
In other words, at intermediate temperatures small vacancy clusters or agglomerates can be formed. Their maximum size is given by the number of vacancies within a volume that is more or less given by L3 - more vacancies are simply not available for any one cluster.
Obviously, what we will get depends very much on the cooling rate and the mobility or diffusivity of the vacancies. We will encounter that again; here is a link looking a bit ahead to the situation where we cool down as fast as we can.
It remains to find out which mix of single vacancies and vacancy clusters will have the smallest free enthalpy, assuming that the total number of vacancies - either single or in clusters - stays constant. This minimum enthalpy for the specific restraint (number of vacancies = const.) and a given temperature then would be the local equilibrium configuration of the system.
How do we calculate this? The simplest answer, once more, comes from using the the mass-action law. We already used it for deriving the equilibrium concentration of the divacancies. And we did not assume that the vacancy concentration was in global thermal equilibrium! The mass action law is valid for any starting concentrations of the ingredients - it simply describes the equilibrium concentrations for the set of reacting particles present. This corresponds to what we called local equilibrium here.
The reaction equation from sub-chapter 2.2.1 was 1V + 1V V2 and in this case this is a valid equation for using the mass action law. The result obtained for the concentration of divacancies with the single vacancy concentration in global thermal equilibrium was
 
c2V  = (c1V)2  ·   z
2
 ·  exp ΔS2V
k
 ·  exp  B2V
kT
 
Don't forget that concentrations here are defined as n/N, i.e. in relative units (e.g. c = 3,5 · 10–5) and not in absolute units, e.g. c = 3,5 · 1015 cm–3.
For arbitrary clusters with n vacancies (1V + 1 V + ... + 1V Vn) we obtain in an analogous way for the concentration cnV of clusters with n vacancies
 
cnV  = (c1V)n  ·   z
2
 ·  exp ΔSnV
k
 ·  exp  BnV
kT
 
with BnV = average binding energy between vacancies in an n-cluster, and c1V = const. concentration of the vacancies (and no longer the thermal equilibrium concentration !).
The essential point now is to realize that these equations still work for local equilibrium! They now describe the local equilibrium of vacancy clusters if a fixed concentration of vacancies is given. The situation now is totally different from global equilibrium. If we consider divacancies for example, we have:
Global equilibrium:
c2V(eq) << c1V(eq) ; and c2V(eq)  rapidly decreases with decreasing temperatures since c1V(eq) decreases.
Local equilibrium:
c2V is increasing with decreasing T since c1V  stays about constant, but we still have the exp+BnV/ kT term that increases with T
Whereas the concentration of clusters may still be small, they now contain most of the vacancies.
Generally speaking, it is always energetically favorable, to put the surplus vacancies in clusters instead of keeping them in solid solution if there is no possibility to annihilate them completely. It thus comes as no surprise that in rapidly cooled down crystals with not to many defects that can act as sinks, we will find some vacancy clusters at room temperature
It also should come as no surprise that the same is true for impurity atoms - vacancy clusters. The equations governing this kind of point defect agglomeration are, after all, quite similar to the equations discussed here.
If you now take the extreme case of a rather perfect Si single crystal (no sinks for point defects), where we do not just have vacancies at thermal equilibrium, but also some relevant concentration of interstitials, interstitial oxygen and substitutional carbon, you might well wonder what one will find at room temperature.
Well - don't wonder! Get to work! It is not all that clear. And even if that puzzle has been solved before you reach productive scientisthood, there is always GaAs, or InP, or SiC, or - well, you will find something left to do, don't worry.
 
Questionaire
Multiple Choice questions to 2.1.1

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