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首页> 外文期刊>Radiochimica Acta: International Journal for Chemical Aspects of Nuclear Science and Technology >Uranium(VI) interaction with pyrite (FeS2): Chemical and spectroscopic studies
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Uranium(VI) interaction with pyrite (FeS2): Chemical and spectroscopic studies

机译:铀与黄铁矿(FeS2)的相互作用:化学和光谱学研究

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The mechanism of uranium(VI) interaction with pyrite was studied by solution chemistry and X-ray Photoelectron Spectroscopy (XPS). Natural pyrite was characterized by X-Ray Diffraction (XRD) and Scanning Electron Microscopy (SEM). After equilibration in 10(-2) moI L-1 NaNO3, pyrite was reacted with uranium(VI) by the batch method in an anoxic glove box (P-O2 < 1 ppm) at ambient temperature. The reaction products of uranium, iron and sulphur were characterized (oxidation state, chemical environment) by XPS. Quantitative analysis revealed that only a few atomic percent of uranium is retained at the pyrite surface. The U4f core level binding energies are consistent with the coexistence of an uranium(VI) species and of uranium in a reduced form. No sulphur oxidation products were observed by XPS, but spectral decomposition of the Fe 2p lines revealed the presence of iron(III) oxide or (oxy)hydroxide. These results seem to point to a redox reaction between uraniurn(VI) and pyrite.
机译:通过溶液化学和X射线光电子能谱(XPS)研究了铀(VI)与黄铁矿相互作用的机理。天然黄铁矿的特征在于X射线衍射(XRD)和扫描电子显微镜(SEM)。在10(-2)Mol L-1 NaNO3中平衡后,在环境温度下,通过分批方法在缺氧手套箱(P-O2 <1 ppm)中使黄铁矿与铀(VI)反应。用XPS对铀,铁和硫的反应产物进行了表征(氧化态,化学环境)。定量分析表明,只有少量原子百分比的铀保留在黄铁矿表面。 U4f核心能级结合能与铀(VI)物种和还原形式的铀共存一致。 XPS未观察到硫氧化产物,但Fe 2p谱线的光谱分解表明存在氧化铁(III)或(氧)氢氧化物。这些结果似乎表明尿嘧啶(VI)与黄铁矿之间存在氧化还原反应。

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