Silica-pillared zirconium phosphate shows both micro- and mesoporous charac
ter, with an average pore dimension of 23 Angstrom after calcination at 480
degreesC. Cu2+ coordinates in solution to the molecular precursor of the s
ilica pillars, 2-aminoethyl-3-aminopropylsiloxane oligomers, and is carried
into the interlayer region on contacting this solution with a-zirconium ph
osphate, where it serves as a probe for the evolution of the intercalated p
hase to a porous pillared solid on calcination. Electron paramagnetic reson
ance spectroscopy shows that the environment of Cu2+ changes from (4 + 2) n
itrogen + oxygen to one containing oxygen only as the organic functions are
eliminated. Above 400 degreesC, (the temperature at which the material sta
rts to exhibit appreciable surface area) and up to 600 degreesC, the e.p.r.
spectrum remains unchanged, and these limits define the temperature region
in which the silica-pillared phosphate is stable. Two copper sites are ide
ntified in the pillared phase. These are considered to correspond to one in
which copper is surrounded by oxygen atoms of the silica pillars, suggesti
ng that part of the Cu2+ forms an integral part of the pillars, and a secon
d related to Cu2+ occluded in the pores and accessible to incoming species
such as water. (C) 2001 Elsevier Science B.V. All rights reserved.