Ch. Pons et al., QUANTIFICATION CURVES FOR XRD ANALYSIS OF MIXED-LAYER 14-ANGSTROM 10-ANGSTROM CLAY-MINERALS/, Clays and clay minerals, 43(2), 1995, pp. 246-254
Using theoretical profiles of diffracted X-ray intensity for interstra
tification between layers having d-spacings around 14.3 Angstrom and 1
0.1 Angstrom, a series of diagrams was derived from which the proporti
on of 14.3 Angstrom layers (W-14) and the probability of passing from
a 14.3 Angstrom layer to a 10.1 Angstrom layer (P-14/10) can be derive
d. W-14 can be derived independently of P-14/10 using the angular dist
ance between reflections situated at 18.2 degrees and 25.4 degrees 2 t
heta (CuK alpha). Once W-14 is determined, P-14/10 may be obtained usi
ng the angular width of the diffuse reflections between 27 degrees and
34 degrees 2 theta. In this case, two different diagrams are proposed
for P-14/10 determination because experimental X-ray patterns show ei
ther one or two diffuse reflections. Comparison of five experimental p
atterns with theoretical patterns calculated using W-14 and P-14/10 Ob
tained using these diagrams indicates that the method can be useful fo
r determining W-14 and P-14/10 in unknown samples. Moreover, the metho
d described is independent of the Lorentz polarization factor and the
layer type. The d-spacings associated with the two kinds of layers, ho
wever, should be similar (+/-1%) to those for which the determinative
diagrams were calculated.