112
MUGGLI AND BACKES
displacementredistributesformicacidonthesurface, which
in effect transports formic acid from high coverage regions
(less-active sites) to low coverage regions (more-active
sites), this model overestimates site 1 coverage and under-
estimates both site 2 coverage and the difference in site
activities. Thus the values reported here represent lower
limits for site 1 activity and site 2 coverage and upper limits
on site 1 coverage and site 2 activity.
CONCLUSIONS
DuringPCOonTiO2, formicacidoxidizestoCO2 inasin-
glestepwithoutforminglong-livedintermediates. Lessthan
one-fourth of the formic acid adsorption sites are highly
active for PCO; these sites are at least 20 times more ac-
tive than other formic acid adsorption sites. Water readily
displaces approximately one-third of a formic acid mono-
layer whereas it does not effectively compete for adsorption
sites with the remaining formic acid. Mass balances showed
that, on average, each adsorbed H2O molecule displaces
one formic acid molecule. Water that is produced during
PCO redistributes adsorbed formic acid on the surface by
displacement. During transient PCO, redistributing surface
coverage transports formic acid from less-active to more-
active sites, which enhances the formic acid oxidation rate.
Adsorbed H2O does not poison the PCO activity of TiO2.
Heating TiO2 to 373 K also redistributes adsorbed formic
acid and the maximum CO2 formation rate during PCO at
373 K was twice that at room temperature.
Effect of Heating
Heating TiO2 from room temperature to 373 K (Fig. 3)
dramatically increased PCO activity; although formic acid
coverage at 373 K was 85% of that at room temperature,
the initial CO2 formation rate doubled. At longer reac-
tion times, the effect of heating was more dramatic. For
example, when one-fourth of a formic acid monolayer re-
mained adsorbed, the normalized CO2 formation rate at
373 K was eight times that at room temperature. This may
indicate that formic acid oxidation is activated and the ac-
tivation energy of the less-active sites is greater than that
of the more-active sites, or formic acid adsorbed at less-
active sites is more readily transported to more-active sites
at 373 K. Onishi et al. (34) studied formic acid decompo-
sition on TiO2. They observed that when part of a formic
acid monolayer was removed at 350 K, an ordered (2 × 1)
formic acid adsorption structure could not be maintained
due to surface diffusion. They proposed that formic acid
may surface diffuse above 350 K and noted that the melt-
ing point of TiHCOO was only 374 K. However, in an
experiment in which the UV lights were turned off for
1800 s and then back on after 180 s of transient PCO at
373 K (data not shown), the CO2 formation rate was the
same before and after the dark period. If the increase in
the PCO rate at 373 K was due to faster formic acid sur-
face diffusion, formic acid would have diffused to more
active sites in the dark and therefore the CO2 formation
rate would have increased when PCO resumed. Therefore,
formic acid surface diffusion does not appear to affect the
formic acid PCO rate at temperatures between 273 and
373 K.
ACKNOWLEDGMENT
Acknowledgment is made to the Donors of the Petroleum Research
Fund, administered by the American Chemical Society, for support of this
research.
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