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Quantification Curves for Mica/Smectite Interstratifications by X-ray Powder Diffraction
1988
Clays and clay minerals
X-ray powder diffraction (XRD) patterns for many interstratified mica/glycolated smectites were calculated by changing combinations of probabilities and transition probabilities of two-component layers. Three basal XRD reflections, 5.1L7.6~ (P l), 8.9 ~ 0.2~ (P2), and 16.1~176 (P3) were selected for the quantification curves. A distinct relationship exists between a20~ (p2 -Pl) and A202 (P3 --P2) which shows systematic changes with expandability at constant Reichweite values. The calculated
doi:10.1346/ccmn.1988.0360307
fatcat:uaqser2awvhifpunch7i534ffu