Jj. Fitzgerald et al., SOLID-STATE AL-27 AND SI-29 NMR AND H-1 CRAMPS STUDIES OF THE THERMALTRANSFORMATIONS OF THE 2 1-PHYLLOSILICATE PYROPHYLLITE/, Journal of physical chemistry, 100(43), 1996, pp. 17351-17360
Solid-state multinuclear magic-angle spinning (MAS) NMR studies of the
thermal transformations of the 2:1 phyllosilicate mineral, pyrophylli
te, over the temperature range 150-1350 degrees C are reported. Al-27
and Si-29 NMR and H-1 CRAMPS techniques have been used to follow the p
rogress of dehydroxylation between 150 and 550 degrees C. At 550 degre
es C, pyrophyllite is completely dehydroxylated in 7 days to pyrophyll
ite dehydroxylate, an aluminosilicate intermediate containing 5-coordi
nate aluminum, on the basis of the MAS Al-27 NMR measurements at 14 T.
MAS Al-27 and CP/MAS (cross-polarization) and SP/MAS (single-pulse) S
i-29 NMR results indicate that the dehydroxylate is formed prior to th
e separation of the silica-alumina layer. At 950 degrees C, the therma
lly induced transformation of pyrophyllite anhydride results in separa
tion of the silica-alumina layer. A transition-alumina-type phase, con
taining 4- and 6-coordinate aluminum, is formed between 950 and 1050 d
egrees C, In addition, a high content of amorphous silica glass and a
small amount of a poorly ordered Si/Al-containing mullite phase forms
between 950 and 1050 degrees C, At 1250-1350 degrees C, the Si-29 NMR
shows that this glassy silica is converted to cristobalite, while the
Al-27 NMR indicates that this process is accompanied by conversion of
octahedral aluminums to tetrahedral aluminums, possibly by incorporati
on of aluminums into an amorphous Si/Al-containing phase. The mechanis
m of dehydroxylation and of the higher temperature transformations of
pyrophyllite dehydroxylate are discussed in light of these multinuclea
r solid-state MAS NMR results.