Spectroscopic and structural properties of synthetic micas on the annite-siderophyllite binary: Synthesis, crystal structure refinement, Mossbauer, and infrared spectroscopy
Gj. Redhammer et al., Spectroscopic and structural properties of synthetic micas on the annite-siderophyllite binary: Synthesis, crystal structure refinement, Mossbauer, and infrared spectroscopy, AM MINERAL, 85(3-4), 2000, pp. 449-465
The effect of the incorporation of Al-Tschermak's molecule to the trioctahe
dral potassium mica annite {K}[Fe-3]<AlSi3>O-10(OH)(2) on local and average
structure has been investigated by hydrothermal synthesis, structure refin
ement of X-ray powder diffraction data. Mossbauer and infrared spectroscopy
. The various types of brackets indicate different structural sites. Sample
s with compositions {K}[Fe3-xAlx]<Al1+xSi3-x>O-10(OH)(2) were prepared by h
ydrothermal techniques. The maximum solubility of Al3+ is limited to x = 0.
92 at 500 degrees C and to x = 0.82 at 700 degrees C. The main factor contr
olling the substitution limits is the ditrigonal distortion of the tetrahed
ral rings. Lattice parameters decrease linearly with increasing Al3+ conten
t of the mica. A considerable decrease of M2-O and nearly no change of M1-O
bond lengths with increasing Al3+ contents is indicative of preferred occu
pation of the M2 site by [Al3+]. Changes in K-O distances are also very pro
nounced and reflect the ditrigonal distortion of the tetrahedral sheet. The
bimodal ferrous quadrupole splitting distribution (QSD) in annite, extract
ed from Mossbauer spectra, becomes narrower and more centered around 2.60 m
m/s with increasing Al3+ contents, and its evolution suggests an increasing
deviation from ideal octahedral coordination of Fe by O, illustrated by th
e increasing octahedral flattening angle psi. The population of individual
QSD components proves that it is impossible to resolve cis and trans M-site
s in micas by Mossbauer spectroscopy. In the hydroxyl stretching region, up
to 7 bands are observed in the infra-red spectra which correspond to OH gr
oups adjacent to 3 Fe2+ (N-bands), to OH groups coordinated by Fe2+, Al3+,
and Fe3+ (I-bands) and to configurations having one octahedral vacancy (V-b
ands). N- and I-type bands are shifted toward lower wavenumbers with increa
sing Al3+ content because of increasing OH ... O-tet interactions.