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Clays and Clay Minerals; December 2002; v. 50; no. 6; p. 799-806
© 2002 Clay Minerals Society
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PREPARATION AND CHARACTERIZATION OF Eu-MAGADIITE INTERCALATION COMPOUNDS

Naoko Mizukami1, Masashi Tsujimura1, Kazuyuki Kuroda1,2 and Makoto Ogawa3,4,*

1 Department of Applied Chemistry, Waseda University, Ohkubo 3-4-1, Shinjuku-ku, Tokyo 169-8555, Japan
2 Kagami Memorial Laboratory for Materials Science and Technology, Waseda University, Nishiwaseda 2-8-26, Shinjuku-ku, Tokyo 169-0051, Japan
3 PRESTO, Japan Science and Technology Corporation (JST)
4 Department of Earth Sciences, Waseda University, Nishiwaseda 1-6-1, Shinjuku-ku, Tokyo 169-8050, Japan

* E-mail address of corresponding author: makato{at}waseda.ac.jp

The intercalation of europium ions (Eu3+) into the interlayer space of a layered silicate, magadiite, was conducted by ion-exchange reactions between magadiite and europium(III) chloride. X-ray diffraction and elemental analysis results indicated that Eu3+ cations were intercalated into the interlayer space of magadiite. The ion exchange between Eu3+ and Na+ occurred preferentially so that the adsorbed Eu3+ amounts were controlled quantitatively. Thermal transformation of the original layered structure was suppressed by the intercalation of Eu3+. The resulting intercalation compounds exhibited photoluminescence arising from the intercalated Eu3+. The luminescence intensity varied in accordance with the amount of Eu3+ absorbed, suggesting that the self-quenching occurred at higher loading levels. The luminescence intensity was also changed by the heat treatment, corresponding to the change in the surroundings of the Eu3+ adsorbed, induced by the removal of the adsorbed water molecules and the hydroxyl groups of the silicate.

Key Words: Europium • Intercalation • Luminescence • Magadiite • Nanocomposite




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T. Okada, Y. Ehara, and M. Ogawa
ADSORPTION OF Eu3+ TO SMECTITES AND FLUORO-TETRASILICIC MICA
Clays and Clay Minerals, August 1, 2007; 55(4): 348 - 353.
[Abstract] [Full Text] [PDF]




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