Sorption behavior of the Pt(II) complex anion on manganese dioxide (δ-MnO2): a model reaction to elucidate the mechanism by which Pt is concentrated into a marine ferromanganese crust
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  • 作者:Mamiko Yamashita Maeno ; Hironori Ohashi ; Kotaro Yonezu…
  • 关键词:Sorption of Pt ; δ ; MnO2 ; XPS ; XAFS ; Ferromanganese crust
  • 刊名:Mineralium Deposita
  • 出版年:2016
  • 出版时间:February 2016
  • 年:2016
  • 卷:51
  • 期:2
  • 页码:211-218
  • 全文大小:587 KB
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  • 作者单位:Mamiko Yamashita Maeno (1)
    Hironori Ohashi (2)
    Kotaro Yonezu (3)
    Akane Miyazaki (4)
    Yoshihiro Okaue (1)
    Koichiro Watanabe (3)
    Tamao Ishida (1)
    Makoto Tokunaga (1)
    Takushi Yokoyama (1)

    1. Department of Chemistry, Faculty of Science, Kyushu University, 6-10-1 Hakozaki, Higashi-ku, Fukuoka, 812-8580, Japan
    2. Faculty of Arts and Science, Kyushu University, 744 Motooka, Nishi-ku, Fukuoka, 819-0395, Japan
    3. Department of Earth Resource Engineering, Faculty of Engineering, Kyushu University, 744 Motooka, Nishi-ku, Fukuoka, 819-0395, Japan
    4. Department of Chemical and Biological Sciences, Faculty of Science, Japan Women’s University, Mejirodai, Bunkyo-ku, Tokyo, 112-8681, Japan
  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Earth sciences
    Geology
    Mineral Resources
    Mineralogy
  • 出版者:Springer Berlin / Heidelberg
  • ISSN:1432-1866
文摘
It is difficult to directly investigate the chemical state of Pt in marine ferromanganese crusts (a mixture of hydrous iron(III) oxide and manganese dioxide (δ-MnO2)) because it is present at extremely low concentration levels. This paper attempts to elucidate the mechanism by which Pt is concentrated into marine ferromanganese crust from the Earth’s continental crust through ocean water. In this investigation, the sorption behavior of the Pt(II) complex ions on the surface of the δ-MnO2 that is a host of Pt was examined as a model reaction. The δ-MnO2 sorbing Pt was characterized by X-ray photoelectron spectroscopy (XPS) and X-ray absorption fine structure (XAFS) to determine the chemical state of the Pt. Hydrolytic Pt(II) complex ions were specifically sorbed above pH 6 by the formation of a Mn-O-Pt bond. XPS spectra and XANES spectra for δ-MnO2 sorbing Pt showed that the sorbed Pt(II) was oxidized to Pt(IV) on δ-MnO2. The extended X-ray absorption fine structure (EXAFS) analysis showed that the coordination structure of Pt sorbed on δ-MnO2 is almost the same as that of the [Pt(OH)6]2− complex ion used as a standard. Therefore, the mechanism for the concentration of Pt in marine ferromanganese crust may be an oxidative substitution (penetration of Pt(IV) into structure of δ-MnO2) by a reduction-oxidation reaction between Pt(II) in [PtCl4-n(OH)n]2− and Mn(IV) in δ-MnO2 through a Mn-O-Pt bond. Keywords Sorption of Pt δ-MnO2 XPS XAFS Ferromanganese crust

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