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Inhibition of Uranium(Ⅵ) Sorption on Titanium Dioxide by Surface Iron(Ⅲ) Species in Ferric Oxide/Titanium Dioxide Systems

机译:氧化铁/二氧化钛体系中表面铁(Ⅲ)对二氧化钛吸附铀(Ⅵ)的抑制作用

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摘要

Uranium (U(Ⅵ)) sorption in systems containing titanium dioxide (TiO_2) and various Fe (Ⅲ)-oxide phases was investigated in the acidic pH range (pH 2.5-6). Studies were conducted with physical mixtures of TiO_2 and ferrihydrite, TiO_2 with coprecipitated ferrihydrite, and with systems where Fe(Ⅲ) was mostly present as crystalline Fe(Ⅲ) oxides. The presence of ferrihydrite resulted in decreased U(Ⅵ) sorption relative to the pure TiO_2 systems, particularly below pH 4, an unexpected result given that the presence of another sorbent would be expected to increase U(Ⅵ) uptake. In mixtures of TiO_2 and crystalline Fe(Ⅲ) oxide phases, U(Ⅵ) sorption was higher than for the analogous mixtures of TiO_2 with ferrihydrite, and was similar to U(Ⅵ) sorption on TiO_2 alone. X-ray absorption spectroscopy of the TiO_2 system with freshly precipitated Fe(Ⅲ) oxides indicated the presence of an Fe(Ⅲ) surface phase that inhibits U(Ⅵ) sorption-a reaction whereby Fe(Ⅲ) precipitates as lepidocrocite and/or ferrihydrite effectively blocking surface sorption sites on the underlying TiO_2. Competition between dissolved Fe(Ⅲ) and U(Ⅵ) for sorption sites may also contribute to the observed decrease in U(Ⅵ) sorption. The present study demonstrates the complexity of sorption in mixed systems, where the oxide phases do not necessarily behave in an additive manner, and has implications for U(VI) mobility in natural and impacted environments where Fe(Ⅲ) (oxyhydr) oxides are usually assumed to increase the retention of U(Ⅵ).
机译:研究了在酸性pH范围(pH 2.5-6)下含二氧化钛(TiO_2)和各种Fe(Ⅲ)-氧化物相的系统中铀(U(Ⅵ))的吸附。研究了TiO_2和三水铁矿的物理混合物,TiO_2与共沉淀的三水铁矿的混合物,以及其中Fe(Ⅲ)主要以结晶Fe(Ⅲ)氧化物形式存在的体系。水铁矿的存在导致相对于纯TiO_2系统,U(Ⅵ)的吸附减少,尤其是在pH低于4的情况下,这是出乎意料的结果,因为预期存在另一种吸附剂会增加U(Ⅵ)的吸收。在TiO_2和结晶的Fe(Ⅲ)氧化物相的混合物中,U(Ⅵ)的吸附高于TiO_2和亚铁水合物的类似混合物,并且与单独在TiO_2上的U(Ⅵ)吸附相似。带有新鲜沉淀的Fe(Ⅲ)氧化物的TiO_2系统的X射线吸收光谱表明,存在抑制Fe(Ⅲ)吸附的反应的Fe(Ⅲ)表面相,该反应使Fe(Ⅲ)沉淀为软铁锰矿和/或三水铁矿。有效地阻止了下面的TiO_2上的表面吸附位。溶解的Fe(Ⅲ)和U(Ⅵ)之间的竞争吸附位点也可能有助于观察到的U(Ⅵ)吸附的减少。本研究证明了混合体系中吸附的复杂性,其中氧化物相不一定以加性方式表现,并且对在自然和受冲击的环境中(通常是Fe(Ⅲ)(羟基)氧化物的U(VI)迁移率具有影响)假定增加U(Ⅵ)的保留。

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  • 来源
    《Environmental Science & Technology》 |2012年第20期|p.11128-11134|共7页
  • 作者单位

    Australian Nuclear Science and Technology Organisation, Locked Bag 2001, Kirrawee DC, NSW 2232, Australia;

    Australian Nuclear Science and Technology Organisation, Locked Bag 2001, Kirrawee DC, NSW 2232, Australia;

    School of Civil and Environmental Engineering, University of New South Wales, Sydney, NSW 2052, Australia;

    School of Pharmacy and Applied Science, La Trobe University, P.O. Box 199, Bendigo, Victoria 3552, Australia;

    Australian Nuclear Science and Technology Organisation, Locked Bag 2001, Kirrawee DC, NSW 2232, Australia;

    School of Pharmacy and Applied Science, La Trobe University, P.O. Box 199, Bendigo, Victoria 3552, Australia;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
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  • 入库时间 2022-08-17 14:03:06

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