The structure and
evolution of Pd species in Pd-exchanged zeolite
materials intended for use as passive NO
x
adsorbers were examined under various pretreatment conditions. Using
in situ CO-diffuse reflectance infrared spectroscopy, Pd structures
were characterized after 500 °C pretreatments in inert (Ar),
water (1–2% H2O in Ar), oxidizing (air), and reducing
(H2, CO) atmospheres. Two zeolites of similar Si/Al ratios
but different framework topologies (Beta, CHA) were found to show
different distributions of Pd species, depending on the reducing agent
used. Reduction in H2 (500 °C; 10% H2 in
Ar) followed by re-oxidation (500 °C; air) led to higher amounts
of single-site Pd ions on Pd-CHA than Pd-Beta, whereas high-temperature
reduction in CO (500 °C; 1000 ppm CO in Ar) followed by re-oxidation
(500 °C; air) led to significant loss of ionic Pd on both Pd-CHA
and Pd-Beta, albeit H2 temperature-programmed reduction
and XPS experiments suggest that this phenomena may be limited to
surface Pd. High-temperature treatments with water (500 °C; 1–2%
H2O in Ar) are shown to form either Pd metal or PdO particles,
with Pd-Beta being more susceptible to these effects than Pd-CHA.
This work suggests that the effects of CO are especially problematic
with respect to the durability of these materials in passive NO
x
adsorption applications, especially in the
case of Beta zeolite.