While conventional quantification procedures require a homogeneous sample in the analysis volume, f ( ρz ) models make it possible to analyze stratified samples, i.e. a succession of thin layers of constant thickness, with a total thickness of no more than a few microns.
For a layer buried between depths ρz
i
and ρz
i+1
containing element A, we can, by definition of f (ρz ), write that the characteristic emergent intensity of the element under consideration coming from layer i is equal to :
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