QPA (quantitative phase analysis) of polycrystalline materials using XRPD (
X-ray powder diffraction) can be performed using the combined Rietveld and
reference intensity ratio (RIR) methods, providing an estimate of both the
crystalline and the amorphous phase in a mixture. Although the accuracy of
estimates of the phase composition of simple ternary or quaternary mixtures
is generally very good, uncertainties remain and bias the accuracy of phas
e determinations in complex systems such as pyroclastic rocks, which may co
ntain two or more zeolite species, a number of other phases (generally up t
o four or five), and glass. The contribution of the incoherent scattering,
biasing accuracy, in the glass determination has been discussed in an earli
er work on the modal analysis of pyroclastic rocks [Gualtieri (1996). Powde
r Diffr. 11, 97-106]. In this work, the assumption of the crystal structure
, the influence of the spike addition, background and atomic (thermal) disp
lacement parameters are discussed. It is shown that the structure-model ass
umption no longer holds for systems containing complex phases such as zeoli
tes, as the accuracy is degraded and, as far as the influence of the added
spike is concerned, there is an underestimation of the glass content with i
ncreasing amounts of added spike. (C) 2000 International Union of Crystallo
graphy Printed in Great Britain - all rights reserved.