Speciation of iodine in solid environmental samples by iodine K-edge XANES: Application to soils and ferromanganese oxides

被引:62
作者
Kodama, Sayuri
Takahashi, Yoshio [1 ]
Okumura, Kazu
Uruga, Tomoya
机构
[1] Hiroshima Univ, Grad Sch Sci, Higashihiroshima, Hiroshima 7398526, Japan
[2] Hiroshima Univ, Lab Multiple Isotope Res Astro & Geochem Evolut, MIRAGE, Hiroshima 7398526, Japan
[3] Tottori Univ, Dept Mat Sci, Tottori 6808552, Japan
[4] Japan Synchrotron Radiat Res Inst, JASRI, SPring 8, Mikazuki, Hyogo 6795198, Japan
关键词
iodine; YANES; soil; speciation;
D O I
10.1016/j.scitotenv.2006.01.004
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
A method was developed for speciation of iodine in solid materials using X-ray absorption near-edge structure (XANES). This method was used to identify the iodine species (mainly inorganic iodine) in environmental samples. It was shown that the XANES spectra of iodide and iodate sorbed within solid materials can be simulated by the linear combination of the spectra of iodide and iodate ions in water. The distribution coefficient (K-d) between soil and water was obtained independently for iodide and iodate, based on iodine speciation both in the solid phase, by XANES, and in the aqueous phase, by HPLC-ICP-MS. It was found that the Kd of iodate is larger than that of iodide by a factor of more than six, showing the more soluble nature of iodide. It was suggested that iodate can form in soil even when iodide is injected into the soil-water system under conditions within the iodide-stable field of the Eh-pH diagram of iodine. This is caused by the much higher affinity of iodate for solid surfaces than iodide. In soil samples under various water saturation conditions, or various Eh conditions, the iodide fraction in water increases with decreasing Eh, which results in an increase in the dissolved total iodine fraction in soil water. The speciation method using XANES was also applied to iodine in a natural soil sample and marine ferromanganese oxides. It is suggested that iodine K-edge XANES is a promising tool for determining the iodide/iodate ratio in natural solid samples, which contributes to better understanding of the behavior of iodine at the Earth's surface. (c) 2006 Elsevier B.V. All rights reserved.
引用
收藏
页码:275 / 284
页数:10
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