THE NATURE OF DIFFRACTION EFFECTS FROM ILLITE AND ILLITE-SMECTITE CONSISTING OF INTERSTRATIFIED TRANS-VACANT AND CIS-VACANT 2 1 LAYERS - A SEMIQUANTITATIVE TECHNIQUE FOR DETERMINATION OF LAYER-TYPE CONTENT/
Va. Drits et Dk. Mccarty, THE NATURE OF DIFFRACTION EFFECTS FROM ILLITE AND ILLITE-SMECTITE CONSISTING OF INTERSTRATIFIED TRANS-VACANT AND CIS-VACANT 2 1 LAYERS - A SEMIQUANTITATIVE TECHNIQUE FOR DETERMINATION OF LAYER-TYPE CONTENT/, The American mineralogist, 81(7-8), 1996, pp. 852-863
Previous work has described the structural and diffraction criteria fo
r distinguishing between tv-1M, cv-1M, and m-1M illite varieties, wher
e tv-1M illite corresponds to a structure with trans vacant (tv) 2:1 l
ayers, cv-1M illite consists of cis-vacant (cv) 2:1 layers, and m-1M i
llites consist of 2:1 layers with random distributions of octahedral c
ations over trans and cis sites within each layer. Detailed analysis o
f calculated and experimental X-ray diffraction (XRD) patterns from il
lites and mixed-layered illite-smectites (I/S) with a range of cis- an
d trans-vacant layer interstratification, and consideration of unit-ce
ll parameters for pure tv-1M and cv-1M provides insight into the natur
e of the diffraction effects from the interlayered structures with dif
ferent types and contents of rotational stacking defects. Structural f
ragments of the 2M(1) and 2M(2) polytypes exist within 1Md structures
in which rotational disorder is dominated by n . 120 and n . 60 degree
s, respectively. Such structural fragments constitute coherent-scatter
ing domains and affect the peak positions of the diagnostic 11l reflec
tions for rotationally disordered I/S and illites in different ways de
pending on the proportion of cis- and trans-vacant 2:1 layers. Simple
techniques that do not require computer programs were developed for th
e semiquantitative determination of the proportion of tv and cv 2:1 la
yers in I/S and illites where such layers are interstratified. These t
echniques may help to reveal the diversity of I/S and illite samples r
elating to the conditions of their formation and transformation.