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Speciation of iodine on biogenic iron oxyhydroxides by I K-edge and LIII-edge XANES
被引:0
|作者:
Kikuchi, Sakiko
[1
]
Kashiwabara, Teruhiko
[2
]
Kurisu, Minako
[2
]
Wakaki, Shigeyuki
[1
,3
]
机构:
[1] Japan Agcy Marine Earth Sci & Technol JAMSTEC, Inst Extra Cutting Edge Sci & Technol Avant Garde, Kochi Inst Core Sample Res, 200 Monobe Otsu, Nankoku, Kochi 7838502, Japan
[2] Japan Agcy Marine Earth Sci & Technol JAMSTEC, Res Inst Marine Resources Utilizat, Submarine Resources Res Ctr, 2-15 Natsushima Cho, Yokosuka, Kanagawa 2370061, Japan
[3] Natl Museum Japanese Hist, Museum Sci Div, Jonaicho 117,Sakura Ku, Chiba 2858502, Japan
基金:
日本学术振兴会;
关键词:
biogenic iron oxyhydroxides;
iodine;
X-ray absorption near-edge structure;
ADSORPTION;
SORPTION;
OXIDES;
IODATE;
FERRIHYDRITE;
EQUILIBRIUM;
MOLYBDENUM;
PREDICTION;
SEDIMENTS;
SOILS;
D O I:
10.1093/chemle/upae023
中图分类号:
O6 [化学];
学科分类号:
0703 ;
摘要:
The host phase of iodine (I) in biogenic iron oxyhydroxides (BIOS) was determined using X-ray absorption near-edge structure (XANES). I K-edge and L-III-edge XANES analyses of BIOS collected from deep-sea hydrothermal environments revealed that the primary form of I in the BIOS is an organic species. Furthermore, L-III-edge XANES fitting implied the dominance of aromatic-bound I among BIOS. Our first observation of organic- trace element association in natural BIOS can explain the enhanced adsorption of I on BIOS compared to synthetic ferrihydrite. This further suggests the importance of various chemistry on this organic-mineral composite for understanding the geochemical cycling of trace elements
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页数:4
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