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Derivation of the Parabolic Rate Law In oxidation processes, parabolic kinetics occurs when the mass gain or oxide growth on a sample is proportional to the square root of time. In general, parabolic kinetics indicates that diffusion of reactants (such as Fe, O, or electrons) through a growing oxide scale is ratedetermining (Kofstad 1966). If the diffusion of Fe ions is rate-determining, the oxidation rate is proportional to the flux of cations through the oxide scale: dx ∝ j Fe dt (1) j Fe = c Fe v Fe (2) The cation flux, j Fe, can be written as where cFe is the concentration in particles cm-3 and v Fe is the velocity of Fe ions in cm s-1 , giving j Fe units of particles cm-2 s-1 . The velocity of a particle or ion in the scale is proportional to the force, F, on the particle: v Fe = B Fe F (3) where BFe is the mobility of the ion. In the case of metallic oxidation, the driving force results from a chemical potential gradient across the oxide scale. Writing the chemical potential as µFe, this force is written as F= dµ Fe dx (4) for an oxide scale with thickness x. Combining equations 3 and 4 yields j Fe = c Fe BFe dµ Fe dx (5) from the relationship µ Fe = µ oFe + k T ln a Fe (6) we can write dµ Fe d ln aFe k T da Fe = kT = dx dx a Fe dx (7) In an ideal system, the concentration, cFe, is equivalent to activity, aFe. Substituting and combining equations, we get j Fe = c Fe B Fe dc k T dc Fe = BFe k T Fe cFe dx dx (8) As shown in equation 1, dx = [constant] j Fe dt (9) so that a combination of equations 1 and 8 gives dc dx = [constant]B Fek T Fe dt dx (10) If we assume that the potential is fixed at each boundary of the oxide scale, we can replace dcFe/dx in equation 10 with ∆cFe/x. We then introduce the parabolic rate constant k’, and set k ' = [constant ]BFe kT∆c Fe (11) Combining equations 10 and 11 then gives dx k ' = dt x (12) xdx = k ' dt (13) Equation 12 can be rewritten as Upon integration of equation 13, x= x t =t x= 0 t =0 ∫ xdx = ∫ k' dt (14) we arrive at the parabolic rate law: x 2 = 2 k 't (15)