The Zr-pillaring of natural hectorite and synthetic laponite clay was
investigated using X-ray diffraction (XRD), Fourier transform infrared
spectroscopy (FTIR) and thermogravimetric analysis (TGA) to character
ize the different substrates. The difference in particle size of both
clays is responsible for their differences in crystallinity, surface a
rea (SA) and micropore volume (mu PV) and consequently for their pilla
red forms too. Pre-adsorption of ethylenediamine in the interlayer spa
ce of laponite is performed in order to reduce the important contribut
ion of edge-to-face and edge-to-edge stacking of the clay layers and c
reating a more homogeneous substrate for pillaring. As is proven by XR
D, TGA and FTIR, ethylenediamine is exchanged completely for the Zr-pi
llaring precursors during the pillaring reaction. Surface areas and mi
cropore volumes of, respectively, 482 m(2)/g and 0.34 cm(3)/g for Zr-p
illared laponite and 171 m(2)/g and 0.064 cm(3)/g for Zr-pillared hect
orite after calcination are obtained. Through pillaring, especially sm
all pores (< 0.71 nm), additional secondary micropores are formed with
laponite while for hectorite, pores over a broad size range are obser
ved. The prepared pillared interlayered clays (PILCs) were tested for
their gas adsorption behaviour. Gas adsorption measurements on Zr-lapo
nite reveal high adsorption capacities for N-2 and O-2 with a low N-2/
O-2 selectivity at 0 degrees C.