Studies on the behavior of Co 2+ and Zn 2+ in the conversion from FeOOH to magnetite in NH 3 (NaOH)–Fe 2+, Co 2+–H 2O medium under hydrothermal conditions

Abstract

Crystalline FeOOH and Zn(II) doped FeOOH samples were prepared by a co-precipitation method using ferrous sulphate heptahydrate, zinc sulphate heptahydrate, ammonia, 3% hydrogen peroxide at 80 °C and pH value 3.0. These samples were characterized by XRD and were also chemically analyzed. The XRD patterns of pure FeOOH matched with that of Zn(II) doped FeOOH sample and showed no shift in their d-values, which indicated that Zn 2+ ions were adsorbed on the surface of FeOOH or on the surface of the crystalline lattice, and were not captured into the ferrite lattice. Chemical analysis showed that the molar ratio of Zn(II)/Fe in Zn(II) doped FeOOH sample was only 0.038 when this ratio was 0.5 in an initial reaction solution. These samples were treated in ammoniacal or sodium hydroxide medium in the presence of ferrous sulphate or cobalt sulphate under hydrothermal conditions. The converted products were analyzed both for ferrous, total iron, cobalt and zinc. Characterization was carried out using instrumental techniques such as SEM, FT-IR, XRD and magnetization characterization. Though the XRD patterns of the converted products showed presence of only magnetite in the NH 3–Fe 2+, Co 2+–H 2O converted medium, the FT-IR spectra and chemical analysis showed an un-reacted FeOOH in the converted product. Even though, the saturation magnetization of this magnetite was higher to 97.489 emu g − 1 . Furthermore, higher temperature increased the concentration of Co 2+ captured into spinel structure. The conversion were restrained in NH 3 concentration of less than 12 g/L and more than 25 g/L. However, increasing of Fe 2+/Co 2+ ratio in the NH 3–Fe 2+, Co 2+–H 2O medium made no distinct difference in the introduction of Co 2+ into spinel structure when concentration of Fe 2+ was enough. Compared with Zn-free FeOOH, it was difficult for Zn-doped FeOOH to convert to magnetite in the NH 3 (NaOH)–Fe 2+–H 2O medium. Furthermore, alkali species were critical in the above conversion. The content of Zn 2+ which was out of Zn-doped FeOOH solid state and entered into the outer solution was more in the NH 3 medium than that of the NaOH medium, but conversion from Zn–FeOOH into magnetite was easy in the NaOH medium. The explanations of above facts were given in the text.