Advice on Analyzing Chloride Ion Penetration Profile Data

(Assumption of a semi-infinite media)
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If at a fixed time, t, the free chloride concentration, C, as a function of depth, x, is available, one can estimate the diffusion coefficient, D, by fitting the following equation to the available data (based on a solution of Fick's 2nd law for a semi-infinite media):
C(x,t)/C(external) = erfc (x/(2.*sqrt(D*t)))
This assumes that C(external) is constant, such as exposure in seawater.

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In practice, C(external) may vary with time and D may vary with distance and time. The model available as part of this distributed knowledge system computes C(x,t) for the case where C(external) varies as a square-wave function and D is a function of distance.

For the case of a two-layer composite, Carslaw and Jaeger have developed a solution for the analogous heat conduction problem. Transformed to mass transfer variables (as performed by Andrade et al), the solution for a semi-infinite media with a constant value of C(external) is given by:

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where b is the thickness of the first layer and D1 and D2 are the diffusion coefficients for the first (surface) and second (bulk) layers.

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