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American Mineralogist; August-September; v. 93; no. 8-9; p. 1384-1392; DOI: 10.2138/am.2008.2628
© 2008 Mineralogical Society of America
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Influence of multi-electron excitation on EXAFS spectroscopy of trivalent rare-earth ions and elucidation of change in hydration number through the series

Atsuyuki Ohta1,*, Hiroyuki Kagi2, Hiroshi Tsuno3, Masaharu Nomura4 and Iwao Kawabe5

1 Geological Survey of Japan, AIST, Tsukuba 305-8567, Japan
2 Geochemical Laboratory, Graduate School of Science, The University of Tokyo, Tokyo 113-0033, Japan
3 Faculty of Education and Human Sciences, Yokohama National University, Kanagawa, 240-8501, Japan
4 Photon Factory, Institute of Materials Structure Science, KEK, Tsukuba 305-0801, Japan
5 Department of Earth and Planetary Sciences, Graduate School of Environmental Studies, Nagoya University, Nagoya 464-8602, Japan

Correspondence: * E-mail: a.ohta{at}aist.go.jp

We have made a detailed study of the extended X-ray absorption fine spectra (EXAFS) at the K edge of aqueous Y ion and at L3 edges of aqueous lanthanide ions and thereby elucidated the systematic changes in their hydration structures. Anomalous peaks arising from double-electron excitation (2p, 4d -> 5d, 5d) appear in the EXAFS signals of La3+-Tb3+ between 5–7 Å–1. We established a removal process of double-electron excitation from EXAFS spectra. Using that process, we confirmed that the intensity and energy position of the extracted double-electron excitation are comparable to previously reported data. The presence of double-electron excitation engenders a smaller error than the errors estimated in the fitting process. Consequently, double-electron excitation does not seriously affect the determination of the structures of REE3+ aquo ions in the first coordination sphere. Subsequent EXAFS analyses of hydrated REE3+ ions suggest that the hydration numbers, the interatomic distances, and the Debye-Waller factors decrease from 9.7, 2.55 Å, and 9.0 x 10–3 Å2 for La3+ to 7.9, 2.31 Å, and 5.7 x 10–3 Å2 for Lu3+. These parameters change as a sigmoid curve with increasing atomic number. The hydration structures of REE3+ ions are inferred to change from the nonahydrated structure for La3+-Nd3+ to the octahydrated structure for Tb3+-Lu3+ through intermediate structures for Sm3+, Eu3+, and Gd3+. In addition, the hydration state of Y3+ closely resembles that of Ho3+ because the two have almost identical ionic radii.

Key Words: EXAFS • rare-earth elements • multi-electron excitation • hydration structure • structural change




This article has been cited by other articles:


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A. Ohta, H. Kagi, M. Nomura, H. Tsuno, and I. Kawabe
Coordination study of rare earth elements on Fe oxyhydroxide and Mn dioxides: Part I. Influence of a multi-electron excitation on EXAFS analyses of La, Pr, Nd, and Sm
American Mineralogist, April 1, 2009; 94(4): 467 - 475.
[Abstract] [Full Text] [PDF]


Home page
American MineralogistHome page
A. Ohta, H. Kagi, M. Nomura, H. Tsuno, and I. Kawabe
Coordination study of rare earth elements on Fe oxyhydroxide and Mn dioxides: Part II. Correspondence of structural change to irregular variations of partitioning coefficients and tetrad effect variations appearing in interatomic distances
American Mineralogist, April 1, 2009; 94(4): 476 - 486.
[Abstract] [Full Text] [PDF]




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