Kinetic adsor
ption isotherms were obtained by gravimetric determination of water adsor
ption into fully hydroxylated meso
porous silicas using sam
ples ex
posed to controlled humidity air at
22±2 °C. Twenty kinetic isotherms at several relative humidities (11, 33, 43, 51, 75, and 85 % ) were obtained with 11 different batches of silica using this sim
ple
procedure to obtain quantitative information on the formation of H
2O adsorbates. The H
2O surface concentrations obtained from the
plateau data of individual kinetic adsor
ption isotherms at 43 and 51 % RH, ty
pically
precise to about ±1 % , show that a com
plete monolayer is formed with negligible second-layer adsor
ption at these relative humidities. This monolayer has a surface concentration of
7.68±0.30 μmol H
2O/m
p>2p>, which is lower than the quasi-equilibrium concentration at these relative humidities obtained by the conventional equilibrium-isotherm
procedure. Com
parison with the
Kiselev–Zhuravlev concentration of silanol grou
ps on fully hydroxylated silicas (
7.6±0.8 μmol SiOH/m
p>2p>) confirms 1:1 H
2O:SiOH stoichiometry of this monolayer. The
presence of
partial-layer structures at
2.85±0.1 and
5.7±0.1 μmol H
2O/m
p>2p> is suggested by isotherms at 11 and 33 % RH, res
pectively, while a bilayer at
l7"">l7&_user=10&_cdi=6857&_rdoc=8&_handle=V-WA-A-W-VU-MsSAYVW-UUA-U-AABZWYBCDW-AABBYZVBDW-CADVYWYCB-VU-U&_acct=C000050221&_version=1&_userid=10&md5=63561b33a35167277877fb578ec8d1ed"" title=""Click to view the MathML source"">p://www.sciencedirect.com/scidirimg/entities/223c.gif"" alt=""not, vert, similar"" border=0>14±1 μmol H
2O/m
p>2p> is suggested by kinetic isotherms at 75 and 85 % RH.