Vanadium-containing MCM-41 materials were prepared by (i) in situ inco
rporation of V during hydrothermal synthesis (denoted as V-MCM-41-syn)
, (ii) chemical vapour deposition of VOCl3 on siliceous MCM-41 (V-MCM-
41-cvd), and (iii) impregnation of siliceous MCM-41 with vanadyl acety
lacetonate (V-MCM-41-imp). A well-ordered hexagonal structure of the m
aterials is revealed from XRD patterns exhibiting four resolved reflec
tions. The fraction of amorphous non-porous by-product obtained from n
itrogen adsorption data increases in the sequence: V-MCM-41-imp approx
imate to 5%<V-MCM-41-cvd approximate to 8%<V-MCM-41-syn approximate to
20%. UV/vis diffuse reflectance spectroscopy (DRS) reveals predominan
tly mononuclear V-V oxide in fourfold tetrahedral coordination owing t
o missing absorptions below 30000 cm(-1) in the dehydrated state for a
ll materials. The content of polynuclear V-V oxide species increases i
n the order: V-MCM-41-syn <V-MCM-41-imp <V-MCM-41-cvd. Reduction by hy
drogen to V-red was monitored by in situ DRS and the fraction of reduc
ible V-V decreases in the sequence: V-MCM-41-imp approximate to 100% >
V-MCM-41-cvd approximate to 67% >V-MCM-41-syn approximate to 14%. The
non-reducible species are assumed to be buried either in the amorphou
s by-product or inside the walls. Photoelectron spectroscopy reveals t
hat the reducible vanadium oxide species are located in the channels o
f the MCM-41 structure. The analysis of the reduction kinetics points
to a small fraction of polynuclear V-V oxide reduced at a tenfold high
er rate. (C) 1998 Elsevier Science B.V. All rights reserved.