Electrochemical route for the synthesis of new nanostructured magnetic mixed oxides of Mn, Zn, and Fe from an acidic chloride and nitrate medium

Citation
F. Torres et al., Electrochemical route for the synthesis of new nanostructured magnetic mixed oxides of Mn, Zn, and Fe from an acidic chloride and nitrate medium, CHEM MATER, 12(10), 2000, pp. 3060-3067
Citations number
23
Categorie Soggetti
Apllied Physucs/Condensed Matter/Materiales Science","Material Science & Engineering
Journal title
CHEMISTRY OF MATERIALS
ISSN journal
08974756 → ACNP
Volume
12
Issue
10
Year of publication
2000
Pages
3060 - 3067
Database
ISI
SICI code
0897-4756(200010)12:10<3060:ERFTSO>2.0.ZU;2-6
Abstract
New nanostructured magnetic Mn-Zn-Fe oxides are electrochemically synthesiz ed as precipitates from chloride + nitrate solutions of pH 1.5 with Mn2+, Z n2+, and Fe2+, or Fe3+ at temperatures between 40 and 80 degreesC using ele ctrodes of commercial iron. The process has been studied using an undivided cell of 100 mt and a stirring batch tank of 700 mt with electrodes of 20 a nd 140 cm(2) area, respectively. Fe2+ is continuously supplied to the solut ion from oxidation of the sacrificial Fe anode, although this ion can be tr ansformed into Fe3+ by reaction with Mn3+, previously formed by anodic oxid ation of Mn2+. An energy cost of ca. 5 kWh kg(-1) is found for the batch ta nk at 35 mA cm(-2). For solutions up to 30 mM Mn2+ and 15 mM Zn2+, magnetic precipitates richer in Fe than in Zn and Mn, with Cu impurity proceeding f rom the anode, are obtained. These materials have an inverse cubic spinel s tructure, being composed of nanoparticles formed by solid solutions of iwak iite, franklinite, magnetite, and maghemite. Magnetically, they behave as s oft ferrites but show lower initial permeability. In contrast, superparamag netic nanoparticles are synthesized by electrolyzing solutions with 110-120 mM Mn2+ and 30 mM Zn2+. These materials with more Mn than Zn and Fe are fo rmed by amorphous mixed oxide, along with two different crystalline phases composed of hetaerolite and a mixture of iwakiite and franklinite, respecti vely.