(
)
H.S. Son et al.rChemical Physics Letters 320 2000 658–664
663
w
x
w
x
studied by Mitchell and Hackett 13 . They observed
states of Fe atoms by various small molecules 19 .
5
Ž
.
that the removal rate of the ground-state Fe a D4
They reported the depletion rate constants for
5
Fe a F5 atoms by O2 and N2O to be 8.3=10y11
and 3.7=10y11 cm3 moleculey1 sy1, respectively.
We also measured the depletion rate constants for
Ž
.
atoms did not increase significantly over the diffu-
sion rate in the presence of O2 or N2O, thereby
concluding that the ground-state Fe atoms were not
reactive toward O2 or N2O. We checked for the
depletion kinetics of the ground-state Fe atoms by
using a photolysis-probe method and reached the
5
Ž
.
the Fe a F5 atoms by O2 and N2O, and obtained
8.6"0.3=10y11 and 3.0"0.2=10y11 cm3 mole-
culey1 sy1, respectively, which are in good agree-
ment with Mitchell and Hackett. They assigned the
depletion rate constants for the metastable Fe atoms
to the collisional relaxation processes based on ki-
netic modeling studies, since they did not succeed to
observe LIF signals from FeO at 578.9 nm. Our
observation of the formation of the ground-state FeO
in this work, however, does not change Mitchell and
Hackett’s assignment of large depletion rate con-
stants for the collisional relaxation processes, be-
cause we observe almost no enhancement of FeO
LIF intensity in spite of increasing the concentration
of metastable Fe atoms by optical pumping.
w
x
same conclusion as Mitchell and Hackett 13 . In
fact, the reaction of the ground-state Fe atoms with
Ž
O2 Eq.
w
is endothermic by 84–92 kJ moly1
Ž ..
2
x
Ž .
3,13–15 , so that the reaction in Eq. 2 is very
unlikely to occur under our experimental conditions.
Fe a5D , g qO
g
2 Ž .
FeO g qO.
Ž .
2
Ž .
Ž
.
4
On the other hand, the reaction of the ground-state
Fe atoms with N2O, Eq. 3 , is highly exothermic by
Ž .
x
;247 kJ moly1 13,14,16 .
Fe a5D , g qN O g
w
FeO g qN g .
Ž . 2 Ž .
3
Ž .
Ž .
Ž
.
4
2
Ryther and Weitz have studied reaction kinetics
xs1–4 photo-fragments
in the gas phase 20 . They have shown that the
triplet state of Fe CO reacts much faster with O2
having triplet ground state than H2 or CO having
singlet ground state. Since the ground states of
Ž .
Ž
.
Ž
.
But it has been reported that the reaction in Eq. 3
does not proceed in an appreciable rate at low tem-
perature 13,16 . The activation energy for the reac-
of unsaturated Fe CO
w
x x
w
x
Ž
.
4
Ž .
tion in Eq. 3 has been reported to be 44.4"1.0
and 45.1"2.3 kJ moly1 by Campbell and Metzger
w
x
w x
Ž
.
Ž
.
w x
16 and Zaslonko and Smirnov 17 , respectively.
Fe CO
xs1–4 photofragments are triplet 21 ,
x
Thus, the ground-state Fe atoms are not considered
to be the source of ground-state FeO molecules
observed in this work. Since the LIF signal from the
FeO orange system is absent unless the photolysis
the much stronger FeO LIF intensity observed in an
O2 mixture in comparision with that in a N2O
mixture seems consistent with the spin selection rule
proposed by Weitz and coworkers 20 . It seems that
reactions of Fe CO
w
.
x
Ž
.
Ž
.
Ž
laser pulse is preceded, the direct reaction of Fe CO
with O2 or N2O in the gas phase is also ruled out for
xs1–4 photofragments,
5
x
Ž
.
most likely those highly unsaturated Fe CO or
2
the source of the ground-state FeO molecules. As the
FeCO, with O2 and N2O are responsible for the
production of FeO in this work.
5
Fe a FJ state lies 6928–8154 cmy1 ;83–97 kJ
Ž
.
Ž
moly1 above the ground state 18 , it is nearly
thermoneutral or slightly exothermic to form
.
w x
Acknowledgements
ground-state FeO molecules in reactions with O2.
3
The Fe a FJ atoms lying 11 976–12 969 cmy1
Ž
.
Ž
;
This work is financially supported in part by the
143–155 kJ moly1 above the ground state are also
energetically viable for the formation of ground-state
FeO molecules. Nevertheless, both metastable states
of the Fe atoms are also ruled out as the source of
the ground-state FeO, because the FeO LIF intensi-
ties remain unchanged in spite of increasing the
concentrations of these states by optical pumping.
Mitchell and Hackett have measured the bimolecular
removal rate constants for a 5D3, a5F5,4 and a3F4,3
.
Ž
Korea Science and Engineering Foundation 96-
.
0501-02-01-3 , and in part by the Ministry of Educa-
Ž
.
tion BSRI-97-3438 .
References
w x
1
M.D. Allen, L.M. Ziurys, J.M. Brown, Chem. Phys. Lett.
Ž
.
257 1996 130.
w x
2
Ž .
R.F. Barrow, M. Senior, Nature 223 1969 1359.