Jt. Kloprogge et al., DEVELOPMENT OF AMMONIUM-SAPONITES FROM GELS WITH VARIABLE AMMONIUM CONCENTRATION AND WATER-CONTENT AT LOW-TEMPERATURES, Clays and clay minerals, 41(1), 1993, pp. 103-110
Ammonium-saponite is hydrothermally grown at temperatures below 300-de
grees-C from a gel with an overall composition corresponding to (NH4)0
.6Mg3Si3.4Al0.6O10(OH)2. The synthetic saponite and coexisting fluid h
ave been characterized by means of X-rav powder diffraction, X-ray flu
orescence. Induced Coupled Plasma-Atomic Emission Spectroscopy, thermo
gravimetric analysis, transmission electron microscopy, CEC determinat
ion using an ammonia selective electrode, and pH measurement. In the c
rystallization model developed, crystallization started with the growt
h of individual tetrahedral layers with an aluminum substitution not c
ontrolled by the Al(IV)/Al(VI) ratio in the gel and hydrothermal fluid
, on which the octahedral Mg layers can grow. During the synthesis, in
dividual sheets stacked to form thicker flakes while lateral growth al
so took place. The remaining Al(VI) partly replaced ammonium as the in
terlayer cation.