We have investigated the interaction of water with Naf-ion exchanged z
eolites of different structures (LTA, FAU, ERI, MOR and MFI) by means
of temperature-programmed desorption (TPD). The non-isothermal desorpt
ion of water shows, depending on the zeolite type, differently structu
red desorption profiles. In every case the profiles have, however, two
main ranges. Using a regularization method, desorption energy distrib
ution functions have been calculated. The desorption energy distributi
ons between 42-60 kJ mol(-1), which can be attributed to a non-specifi
c interaction of water, show two clearly distinguished energy ranges.
The water desorption behaviour of this range correlates with the elect
ronegativity of the zeolites and the average charge of the lattice oxy
gen atoms calculated by means of the electronegativity equalization me
thod (EEM). The part of the desorption energy distributions in the ran
ge of 60-90 kJ mol(-1), reflecting interactions of water with Na+ cati
ons, shows two more or less pronounced maxima. In agreement with vibra
tional spectroscopic studies in the far infrared region, it may be con
cluded that all samples under study possess at least two different cat
ion sites.