Toczydłowska Diana, Kędra-Królik Karolina, Nejbert Krzysztof, Preočanin Tajana, Rosso Kevin M, Zarzycki Piotr
Institute of Physical Chemistry, 44/52 Kasprzaka, Warsaw, Poland.
Phys Chem Chem Phys. 2015 Oct 21;17(39):26264-9. doi: 10.1039/c5cp03106k.
The electrochemical signatures of Fe(II) interactions with iron(III) oxides are poorly understood, despite their importance in controlling the amount of mobilized iron. Here, we report the potentiometric titration of α,γ-Fe2O3 oxides exposed to Fe(II) ions. We monitored in situ surface and ζ potentials, the ratio of mobilized ferric to ferrous, and the periodically analyzed nanoparticle crystal structure using X-ray diffraction. Electrokinetic potential reveals weak but still noticeable specific sorption of Fe(II) to the oxide surface under acidic conditions, and pronounced adsorption under alkaline conditions that results in a surface potential reversal. By monitoring the aqueous iron(II/III) fraction, we found that the addition of Fe(II) ions produces platinum electrode response consistent with the iron solubility-activity curve. Although, XRD analysis showed no evidence of γ-Fe2O3 transformations along the titration pathway despite iron cycling between aqueous and solid reservoirs, the magnetite formation cannot be ruled out.
尽管Fe(II)与铁(III)氧化物的相互作用在控制可移动铁的含量方面具有重要意义,但其电化学特征仍未得到充分理解。在此,我们报告了暴露于Fe(II)离子的α,γ-Fe2O3氧化物的电位滴定。我们原位监测了表面和ζ电位、可移动的三价铁与二价铁的比例,并使用X射线衍射定期分析纳米颗粒晶体结构。动电电位显示,在酸性条件下Fe(II)对氧化物表面有微弱但仍明显的特异性吸附,而在碱性条件下有显著吸附,导致表面电位反转。通过监测水相中铁(II/III)的比例,我们发现添加Fe(II)离子会产生与铁溶解度-活度曲线一致的铂电极响应。尽管XRD分析表明,尽管铁在水相和固相储库之间循环,但沿滴定途径没有γ-Fe2O3转变的证据,但不能排除磁铁矿的形成。