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Observation and Photoelectron Spectroscopic Study of Novel Mono ...

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<strong>Mono</strong>- <strong>and</strong> Diiron Oxide Molecules J. Am. Chem. Soc., Vol. 118, No. 22, 1996 5301complex. The Fe 2 O 3 isomer may consist <strong>of</strong> a Fe 2 O-O 2complex or Fe 2 -O 3 complex. Similarly, the Fe 2 O 4 <strong>and</strong> Fe 2 O 5isomers may also consist <strong>of</strong> O 2 or O 3 units. All these isomersseem to yield rather broad features in the photoelectron spectra,consistent with their weakly bound nature. In some sense, theseO 2 complexes may be more interesting because they may mimicthe properties <strong>of</strong> those O 2 complexes formed in oxygen transportsystems or organometallic-O 2 complexes, that are precursorsfor the cleaving <strong>of</strong> the O-O bond. 17SummaryWe study two series <strong>of</strong> novel iron oxide molecules, FeO y (y) 1-4) <strong>and</strong> Fe 2 O y (y ) 1-5), using anion photoelectronspectroscopy. Important electronic <strong>and</strong> vibrational structuresare obtained, providing unique information about the structures<strong>and</strong> bonding <strong>of</strong> these molecules. For both series, sequentialoxidation behaviors are observed, as inferred from the near linearincrease <strong>of</strong> the electron affinity versus the number <strong>of</strong> O atoms.An oxidation saturation is observed at FeO 3 , consistent withthe known maximum oxidation state <strong>of</strong> the Fe atom. In bothseries, the photoelectron spectra are observed to become simpleras the number <strong>of</strong> O atoms increases. This is consistent with acharge transfer picture where the electrons are sequentiallytransferred from the Fe atoms to the increasing O atoms, yieldinga simpler electronic structure for the higher oxides because theO-derived orbitals all lie deeper in energy <strong>and</strong> cannot beaccessed by the photon energies used. The structures <strong>of</strong> the(38) Goldberg, N.; Iraqi, M.; Koch, W.; Schwarz, H. Chem. Phys. Lett.1994, 225, 404-409. Bencivenni, L.; Pelino, M.; Ramondo, F. J. Mol.Struct. (Theochem) 1992, 253, 109-120. Snyder, L. C.; Raghavachari, K.J. Chem. Phys. 1984, 80, 5076-5079.(39) Nicholas, J. B.; Fan, J.; Wu, H.; Colson, S. D.; Wang, L. S. J. Chem.Phys. 1995, 102, 8277-8280.monoiron series are found to change from a C 2V FeO 2 to a D 3hFeO 3 , <strong>and</strong> finally to a C 2V FeO 4 that contains an O-O bondsince the oxidation state <strong>of</strong> Fe is already saturated at FeO 3 . ThatFeO 4 must contain an O-O unit is also evidenced by observation<strong>of</strong> photodissociation <strong>of</strong> the parent FeO - 4 anion, which canlose an O 2 under high laser fluences to give rise to a broadFeO - 2 feature. For the diiron series, all the spectra are observedto be quite similar, each containing a rather prominent groundstate peak, followed by one or two excited state features.Isomers are also observed for the Fe 2 O - y series when y > 1.These isomers are particularly abundant for Fe 2 O - 2 <strong>and</strong> Fe 2 O- 3<strong>and</strong> complicate the observed spectra. These isomers areproposed to be complexes involving O 2 or O 3 units. For themain oxide sequence, the electron affinity is observed to increasewith the number <strong>of</strong> O atoms. The oxidation is observed not tobe saturated at Fe 2 O 5 , agreeing with the maximum knownoxidation state <strong>of</strong> the Fe atom. Possible structures are proposedfor these oxide molecules, consistent with the experimentalobservations, which provide stringent tests for any theoreticalcalculations that can more completely elucidate the structure<strong>and</strong> bonding <strong>of</strong> these novel oxide molecules.Acknowledgment. We thank Dr. L. Lou for valuablediscussions <strong>and</strong> Pacific Northwest National Laboratory/U.S.Department <strong>of</strong> Energy, Basic Energy Sciences for the development<strong>of</strong> the cluster-PES apparatus. Support for this study fromthe National Science Foundation (Grant No. CHE-9404428) isgratefully acknowledged. This work was performed at PacificNorthwest National Laboratory, operated for the U.S. Department<strong>of</strong> Energy by Battelle under contract DE-AC06-76RLO1830.JA954153B

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