A systematic investigation has been undertaken for tailoring the micro
pore structure of the pillared clay. Besides the type of metal oxide (
e.g. Al2O3 vs. ZrO2) being used as the pillars, the important factors
for determining the micropore structure are OH/Al ratio (for Al2O3-pil
lared clay), calcination temperature and the starting clay. The effect
of the cation exchange capacity (CEC) of the clay on the microporous
structure (and consequently the adsorption properties) is reported for
the first time. Two clays with widely different CECs are used: Arizon
a montmorillonite (CEC=1.40 mequiv./g) and Wyoming montmorillonite (CE
C=0.76 mequiv./g). The interlayer spacings of the pillared clays from
these different clays are essentially the same, since the interlayer s
pacing is controlled by the sizes of the oligomers that intercalate be
tween the clay layers. However, the pillar density in the pillared cla
y is substantially higher with a high CEC in the starting clay, and is
shown to be approximately proportional to the CEC. Consequently, the
interpillar spacing is substantially lower resulting from the higher C
EC. The CH4 adsorption on the pillared clay is nearly doubled by the s
maller interpillar spacing, due to the back-to-back overlapping potent
ial in the micropores. The N-2 adsorption was not significantly influe
nced because of its low polarizability (hence low inductive potential)
. Increasing the calcination temperature of the Al2O3-pillared clay fr
om 400 degrees C to 600 degrees C can decrease the interlayer spacing,
but only by 1 Angstrom (from 8.7 Angstrom to 7.7 Angstrom). The CH4/N
-2 adsorption ratio of 2.35 is reached on the Al2O3-pillared Arizona c
lay that is calcined at 600 degrees C. Finally, the surface and pore v
olume are influenced by the OH/Al ratio (or pH) during pillaring, sinc
e this ratio determines the size and charge of the oligomers. A peak s
urface area is reached at OH/Al=2.2.