Journal of the American Chemical Society
Communication
3629. (b) Chufan
́
, E. E.; Puiu, S. C.; Karlin, K. D. Acc. Chem. Res. 2007,
AUTHOR INFORMATION
Corresponding Author
■
40, 563. (c) Chishiro, T.; Shimazaki, Y.; Tani, F.; Tachi, Y.; Naruta, Y.;
Karasawa, S.; Hayami, S.; Maeda, Y. Angew. Chem., Int. Ed. 2003, 42,
2788.
Present Addresses
(10) Scott, R. A. In Physical Methods in Bioinorganic Chemistry:
Spectroscopy and Magnetism; Que, L., Jr., Ed.; University Science
Books: Sausalito, CA, 2000; pp 465−503.
§F.L.: Brookhaven National Laboratory, Upton, NY 11973.
∥K.M.V.H.: Harvey Mudd College, Claremont, CA 91711.
(11) We attempted to include in fits of 3 a Sc scatterer at ∼3.7 Å. Fits
13 and 14 in Table S2 show that a Sc scatterer at 3.8 Å with a
reasonable Debye−Waller factor (σ2 ≈ 4) could be added but gave
only a slight improvement in the goodness of fit. Similar results were
obtained in the EXAFS analysis of a Sc−O−Co complex (see: Pfaff, F.
F.; Kundu, S.; Risch, M.; Pandian, S.; Heims, F.; Pryjomska-Ray, I.;
Haack, P.; Metzinger, R.; Bill, E.; Dau, H.; Comba, P.; Ray, K. Angew.
Chem., Int. Ed. 2011, 50, 1711 ).
Notes
The authors declare no competing financial interest.
ACKNOWLEDGMENTS
■
This work was supported by the National Science Foundation
(Grant CHE1058248 to L.Q.) and the National Institutes of
Health (Grant EB001475 to E.M. and postdoctoral fellowship
GM093479 to K.M.V.H.). F.L. acknowledges a doctoral
dissertation fellowship from the University of Minnesota.
XAS data were collected at beamline X3B of the National
Synchrotron Light Source at the Brookhaven National
Laboratory and beamline 7-3 of the Stanford Synchrotron
Radiation Lightsource, both supported by NIH and DOE. We
thank Dr. Jason England and Ms. Jennifer Bigelow for
assistance and discussions.
(12) At first glance, the 50 cm−1 upshift in the Fe−O vibration in
going from 2 to 3 may appear to contradict the observed lengthening
of the Fe−O bond distance deduced from the EXAFS analysis, but the
18O shifts found for the respective Fe−O vibrations were quite
different (−15 vs −23 cm−1). The downshift for 3 is as calculated for a
diatomic Fe−O oscillator, but the smaller shift for 2 indicates mixing
of the diatomic Fe−O vibration with other vibrational modes. Thus,
the use of a direct comparison of the frequencies to deduce the Fe−O
bond distance is not valid in this case.
(13) Yao, S.; Xiong, Y.; Vogt, M.; Grutzmacher, H.; Herwig, C.;
̈
Limberg, C.; Driess, M. Angew. Chem., Int. Ed. 2009, 48, 8107.
(14) A related Fe3+−(μ-η2:η2-O2)−H+ core was postulated by Nam
for a short-lived (<2 ms) species (λmax = 527 nm) observed at −40 °C
upon treatment of 2 with strong acid in its conversion to 5.7b
(15) (a) Girerd, J.-J.; Banse, F.; Simaan, A. J. Struct. Bonding 2000, 97,
145. (b) Roelfes, G.; Vrajmasu, V.; Chen, K.; Ho, R. Y. N.; Rohde, J.-
U.; Zondervan, C.; la Crois, R. M.; Schudde, E. P.; Lutz, M.; Spek, A.
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dx.doi.org/10.1021/ja402645y | J. Am. Chem. Soc. XXXX, XXX, XXX−XXX