18178 J. Phys. Chem., Vol. 100, No. 46, 1996
Yamakata et al.
band. Therefore our assignment will be more reasonable. It
should be noted that the peaks of δ(CH), the out-of-plane
deformation band (π(CH)), and νa(OCO) were absent. Taking into
account of the surface selection rule of IRAS, the C-H bond
was regarded as being perpendicular to the surface.
The presence of gaseous or adsorbed hydrogen did not lead
to any noticeable change in the IRA spectrum of formate,
suggesting that the coadsorption of hydrogen on formate-covered
Ni(110) did not cause any significant change in IRA spectra.
Isotope Exchange Reaction of Formate on Ni(110). When
the HCOO-covered surface was exposed to D2 (7 × 10-6 Torr),
the intensity of the ν(CH) (2943 cm-1) and the νs(OCO) (1365
cm-1) bands commenced to decrease, and new bands assigned
to the CD stretching (ν(CD)) and the νs(OCO) bands of DCOO(a)
species appeared at 2188 and 1327 cm-1, respectively, as shown
in Figures 3 and 4. When the D2 gas was replaced by H2 after
the ν(CH) band almost disappeared, the reverse phenomenon was
observed; the ν(CH) band reappeared, and the initial peak intensity
of ν(CH) was recovered completely at the expense of the ν(CD)
band. The quantitative analysis of the process with normaliza-
tion taking into account of the absorption coefficients (ꢀCD/ꢀCH
) 2.1) is shown in Figure 5. The total coverage of formate
(HCOO(a) + DCOO(a)) was confirmed to be constant during
the isotope exchange reaction, i.e., no side reactions such as
decomposition or desorption occurred.
Figure 1. Temperature-programmed desorption (TPD) spectra of
formic acid adsorbed on Ni(110) surface at 113 K.
Figure 2. IRAS spectrum of formate adsorbed on a Ni(110) surface
at 300 K.
Dipole-Dipole Interaction of the νs(OCO) Band. As
shown in Figures 3 and 4, the peak position of the νs(OCO) band
of HCOO(a) and DCOO(a) shifted as the reaction proceeded,
while those of the ν(CH) and ν(CD) bands stayed at the same
positions. Figure 6 is the plot against the coverage of the peak
positions of the νs(OCO) band of HCOO(a) and DCOO(a), where
the coverage was estimated from the intensities of the ν(CH) and
ν(CD) bands shown in Figure 3. The peak positions shifted
almost linearly with the coverage by about 7 and 10 cm-1 for
HCOO(a) and DCOO(a), respectively.
The frequency shift of the νs(OCO) mode of HCOO(a) and
DCOO(a) was attributed to the dipole-dipole coupling among
the same isotope species.21,22 The peak shift due to the dipole-
dipole coupling has been reported for the ν(CO) band of
CO(a),21-23 νs(OCO) band of formate,16 and ν(CO) band of
methoxy.24,25 The linear dependence of the presently observed
peak shift on the coverage seems to suggest that the isotope
exchange reaction on the Ni(110) surface proceeded homoge-
neously.21,22,26 In other word, islands of HCOO(a) and DCOO-
(a) were not formed during the exchange reaction.
The intensities of the νs(OCO) bands were much larger than
those of the ν(CH) and ν(CD) bands which have the linear
relationship between them in intensity (not shown), and the
distinct and linear shift of the νs(OCO) band with the coverage
was used to evaluate the coverage in the subsequent analysis,
as a more precise method than that calculated by the peak
intensities.
Kinetic Analysis of Isotope Exchange Reaction by IRAS.
The kinetics of the isotope exchange reaction is discussed on
the Ni(110) surface with full coverage of formate. The rates
of the isotope exchange reactions are defined as follows:
ation after dosing a certain amount of hydrogen. Since the
exchange reaction does not proceed in the absence of gaseous
hydrogen, the change of IRA spectra gives the reliable rate of
isotope exchange reaction.
3. Results and Discussion
TPD of Formic Acid on Ni(110). The TPD spectra of H2,
H2O, CO, CO2, and HCOOH from the formic acid adsorbed on
Ni(110) at 110 K are shown in Figure 1. The desorption peak
of HCOOH (m/e ) 46) around 185 K was assigned to the
desorption from the second layer or multilayer of formic acid
because this peak increased without saturation by increasing
the exposure. The other peaks of H2, H2O, CO, and CO2 at
185 K were assigned to the cracking of HCOOH.
A broad desorption peak of hydrogen was observed at
250∼320 K and was attributable to the dissociation of the
hydroxyl group of formic acid to form formate. The desorption
peaks of CO2 and H2 at around 360 K were due to the
dehydrogenation of formate as was reported previously, while
the desorption peak of CO at around 440 K was attributed to
the dehydration of formate.6-8 H2O should be produced
simultaneously in the dehydration but was not detected in our
experiment presumably because of the high background signal
of H2O from the wall of the chamber. The results indicated
that the decomposition of formate started at 330 K. Therefore
the CH/CD isotope exchange reaction was performed between
290 and 305 K.
IRAS Spectra of Formate on Ni(110). The IRA spectrum
of formate on Ni(110) surface at 300 K is shown in Figure 2.
Four peaks observed at 779, 1365, 2854, and 2943 cm-1 are
assigned to the OCO deformation band (δ(OCO)), the symmetric
CO stretching band (νs(OCO)), the combination band of the in-
plane CH deformation band (δ(CH)) and the asymmetric CO
stretching band (νa(OCO)), and the CH stretching band (ν(CH)),
respectively. The assignments are summarized in Table 1 along
with the values reported on other metal surfaces.16-20 The peaks
at 2840 and 2944 cm-1 have been assigned to the ν(CH) and the
combination band by Haq et al.,13 respectively, which is different
from the present one. The combination band enhanced by Fermi
resonance should not be more intense than the fundamental ν(CH)
dθHCOO
rHD ) -
rDH ) -
) k′′ θmHCOOPnD
(1a)
(1b)
HD
2
dt
dθDCOO
dt
) k′′ θmDCOO PnH
DH
2
where r, k′′, θHCOO, θDCOO, PD , and PH are the rate of the
2
2
exchange, apparent rate constant, coverage of HCOO(a) and
DCOO(a), and pressure of D2 and H2, respectively. The