H. Vali et al., A TEM-BASED DEFINITION OF 2-1 LAYER SILICATES AND THEIR INTERSTRATIFIED CONSTITUENTS, The American mineralogist, 79(7-8), 1994, pp. 644-653
The layer structure and chemical composition of individual packets of
2:1 layer silicates in illitic materials from various environments hav
e been studied with analytical high-resolution electron microscopy usi
ng ultrathin sections treated with n-alkylammonium. Individual packets
consist of a polar or nonpolar structure, as judged by the response t
o treatment with n-alkylammonium. The status of illite-smectite mixed-
layers attributed to these materials is found to reflect the compositi
on and arrangement of polar and nonpolar 2:1 layer silicates. The natu
re of the 2:1 mixed-layer silicate thus cannot be ascribed to a mixtur
e of illite and smectite layers. In our opinion, a definition based on
TEM reflects the true nature of mixed-layer materials more accurately
than one based on XRD: it leads us (1) to distinguish among different
types of expandable and nonexpandable components; (2) to document var
iations in the density of interlayer charge of the expandable componen
ts, which are not detectable by XRD; (3) to distinguish between expand
able and nonexpandable illite, which do not respond differently to eth
ylene glycol treatment; (4) to distinguish between fundamental particl
es and short-range ordered structures; (5) to relate the ordering of t
he T-O-T layers to the chemical composition, as measured directly by T
EM (XRD study of oriented samples gives information on the interlayer
spacing only); and (6) to characterize all types of particles present
(not only the coherent sequences, as given by XRD).