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利用蒙脱石粘土模板合成高反应性的亚纳米零价铁。

Synthesis of highly reactive subnano-sized zero-valent iron using smectite clay templates.

机构信息

Department of Crop and Soil Sciences, Michigan State University, East Lansing, Michigan 48824, USA.

出版信息

Environ Sci Technol. 2010 Jun 1;44(11):4258-63. doi: 10.1021/es903801r.

Abstract

A novel method was developed for synthesizing subnano-sized zero-valent iron (ZVI) using smectite clay layers as templates. Exchangeable Fe(III) cations compensating the structural negative charges of smectites were reduced with NaBH(4), resulting in the formation of ZVI. The unique structure of smectite clay, in which isolated exchangeable Fe(III) cations reside near the sites of structural negative charges, inhibited the agglomeration of ZVI resulting in the formation of subnanoscale ZVI particles in the smectite interlayer regions. X-ray diffraction revealed an interlayer spacing of approximately 5 A. The non-structural iron content of this clay yields a calculated ratio of two atoms of ZVI per three cation exchange sites, in full agreement with the X-ray diffraction (XRD) results since the diameter of elemental Fe is 2.5 A. The clay-templated ZVI showed superior reactivity and efficiency compared to other previously reported forms of ZVI as indicated by the reduction of nitrobenzene; structural Fe within the aluminosilicate layers was nonreactive. At a 1:3 molar ratio of nitrobenzene/non-structural Fe, a reaction efficiency of 83% was achieved, and over 80% of the nitrobenzene was reduced within one minute. These results confirm that non-structural Fe from Fe(III)-smectite was reduced predominantly to ZVI which was responsible for the reduction of nitrobenzene to aniline. This new form of subnanoscale ZVI may find utility in the development of remediation technologies for persistent environmental contaminants, for example, as components of constructed reactive domains such as reactive caps for contaminated sediments.

摘要

开发了一种使用蒙脱石粘土层作为模板合成亚纳米零价铁 (ZVI) 的新方法。用 NaBH 4 还原补偿蒙脱石结构负电荷的可交换 Fe(III) 阳离子,从而形成 ZVI。蒙脱石粘土的独特结构中,孤立的可交换 Fe(III) 阳离子位于结构负电荷的位置附近,抑制了 ZVI 的聚集,从而在蒙脱石层间区域形成了亚纳米级的 ZVI 颗粒。X 射线衍射显示层间距约为 5 Å。这种粘土的非结构铁含量计算出 ZVI 与三个阳离子交换位点的比例为两个原子,与 X 射线衍射 (XRD) 结果完全一致,因为元素 Fe 的直径为 2.5 Å。粘土模板 ZVI 的反应性和效率优于其他先前报道的 ZVI 形式,这表明其能够还原硝基苯;层状铝硅酸盐中的结构 Fe 没有反应活性。在硝基苯/非结构 Fe 的摩尔比为 1:3 的情况下,达到了 83%的反应效率,超过 80%的硝基苯在一分钟内被还原。这些结果证实,来自 Fe(III)-蒙脱石的非结构 Fe 主要还原为 ZVI,这是硝基苯还原为苯胺的原因。这种新形式的亚纳米 ZVI 可能在开发持久性环境污染物修复技术方面具有应用价值,例如作为污染沉积物反应帽等构建反应区的组成部分。

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