Ma. Vicente et al., CHARACTERIZATION OF THE SOLIDS OBTAINED BY PILLARING OF GRIFFITHITE (HIGH IRON CONTENT SAPONITE) WITH AL-OLIGOMERS, Clays and clay minerals, 45(5), 1997, pp. 761-768
Griffithite, a high Fe content saponite (Griffith Park, California) wa
s pillared with Al polymeric solutions, using different Al/clay ratios
. The cation exchange began when Al-polycation solutions were added, b
eing completed during the dialysis of the samples. Pillared solids wer
e obtained by calcination of intercalated precursors at 500 degrees C.
The content of Al2O3 increased from 7.35% in the natural griffithite
to about 14% in the pillared samples, equivalent to the fixation of ab
out 1.4 mmol Al per g of clay. The surface areas of the pillared griff
ithite were between 230-300 m(2) g(-1). The intercalation and pillarin
g of griffithite were easier than that of a less-crystalline nonferrou
s saponite.