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Structural study of Fe(II) adsorption on hematite(1(1)over-bar02)

机译:铁(II)在赤铁矿上的吸附结构研究(1(1)over-bar02)

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摘要

The structure of alpha-Fe2O3(1 (1) over bar 02) reacted with Fe(II) under anoxic conditions was studied using crystal truncation rod (CTR) diffraction. The CTR results show the crystalline termination of alpha-Fe2O3(1 (1) over bar 02) is modified due to adsorption of Fe(II) at crystallographic lattice sites. In addition, the binding sites for adsorbed Fe are similar for all studied conditions: reaction for 2 It at pH 5.0, for 34 d at pH 5.0, and for 5.5 h at pH 7.0. The occupancy of adsorbed Fe increases with both reaction time and pH, which is consistent with typical cation adsorption behavior on iron (hydr)oxide surfaces. The metal-oxygen bond lengths of the (ordered) surface Fe atoms are characteristic of Fe(III), which provides indirect evidence for oxidation of adsorbed Fe(II) and is consistent with recent studies indicating that Fe(Ill)-hydroxides are effective oxidants for dissolved ferrous iron. Grazing-incidence X-ray diffraction measurements indicate that no crystalline surface reaction products formed during the course of Fe(II) reaction. Overall, the structural characterization of the Fe(II) adsorption reaction results in an enhanced understanding of how reduced iron affects the structure, stability and reactivity of hematite. (C) 2008 Elsevier Ltd. All rights reserved.
机译:使用晶体截断棒(CTR)衍射研究了在缺氧条件下与Fe(II)反应的α-Fe2O3(1(1)在棒02上)的结构。 CTR结果表明,由于Fe(II)在晶体晶格位点处的吸附,α-Fe2O3(1(1)在bar 02)上的结晶终止被修饰。此外,在所有研究的条件下,吸附的Fe的结合位点都相似:在pH 5.0下2 It反应,在pH 5.0下34 d反应和在pH 7.0下5.5 h的反应。 Fe的吸收率随反应时间和pH值的增加而增加,这与(氢氧化)铁表面的典型阳离子吸附行为一致。 (有序的)表面Fe原子的金属-氧键长度是Fe(III)的特征,这为吸附的Fe(II)的氧化提供了间接证据,并且与最近的研究表明氢氧化Fe(III)有效溶解亚铁的氧化剂。掠入射X射线衍射测量表明在Fe(II)反应过程中没有形成结晶表面反应产物。总体而言,Fe(II)吸附反应的结构表征导致人们对铁还原如何影响赤铁矿的结构,稳定性和反应性的认识得到增强。 (C)2008 Elsevier Ltd.保留所有权利。

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