Mn, Fe, Zn and As speciation in a fast-growing ferromanganese marine nodule

被引:138
作者
Marcus, MA
Manceau, A
Kersten, M
机构
[1] Lawrence Berkeley Lab, Berkeley, CA 94720 USA
[2] Univ Grenoble 1, LGIT, Environm Geochem Grp, F-38041 Grenoble 9, France
[3] CNRS, F-38041 Grenoble 9, France
[4] Univ Mainz, Inst Geosci, D-55099 Mainz, Germany
关键词
D O I
10.1016/j.gca.2004.01.015
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The speciation of Mn, Fe, As, and Zn in a fast-growing (0.02mm/yr), shallow-marine, ferromanganese nodule has been examined by micro X-ray fluorescence, micro X-ray diffraction, and micro X-ray absorption spectroscopy. This nodule exhibits alternating Fe-rich and Mn-rich layers reflecting redox variations in water chemistry. Fe occurs as two-line ferrihydrite. The As is strictly associated with Fe and is mostly pentavalent, with an environment similar to that of As sorbed on or coprecipitated with synthetic ferrihydrite. The Mn is in the form of turbostratic birnessite with similar to10% trivalent manganese in the layers and probably similar to8% corner-sharing metal octahedra in the interlayers. The Zn is enriched on the rim of the nodule, associated with Mn. The Zn is completely (>90%) tetrahedrally coordinated and sorbed in the interlayers of birnessite on vacant layer Mn sites. The Zn and Mn species are similar to ones found in soils, suggesting common structural principles despite the differing formation conditions in these systems. Copyright (C) 2004 Elsevier Ltd.
引用
收藏
页码:3125 / 3136
页数:12
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