Lk. Sha et Bw. Chappell, MULTISITE ORDER-DISORDER KINETICS IN CRYSTALLINE SOLIDS - A GENERALIZED FORMULATION, The American mineralogist, 82(3-4), 1997, pp. 325-336
Many crystalline solids have multiple nonequivalent sites among which
different atoms show substitutional long-range order-disorder phenomen
a. The order-disorder kinetics of an atom among any n nonequivalent si
tes in a crystal can be described by the equation x(i)=c(il)+(j=2)Sigm
a(n) c(ij)(t)e(lambda jt) where x, is the site occupancy of the atom a
t site s(i), n is the number of nonequivalent sites, lambda(j)(lambda(
j)=0) is constant at a given temperature, pressure, and total composit
ion of the crystal, and c(ij)(t) is constant or polynomial in t. Four
theorems governing a multi-site order-disorder process have been prove
d, requiring that lambda(j) must be either zero (only lambda(l)=0), a
negative real number, or a complex-valued quantity with the real part
being a nonpositive number. The kinetic model becomes constrained and
naturally complies with crystal-chemical conditions when the mole numb
er per formula unit is chosen as the unit of all site-occupancy variab
les, or site multiplicities are explicitly incorporated into the model
. When the mole fraction is directly used as the unit, the model becom
es unconstrained, but it is a valid treatment that is as equally appli
cable to the multi-site order-disorder kinetics as the constrained mod
el.