Department of Civil and Environmental Engineering, University of Western Ontario, Spencer Engineering Building, London, ON N6A 5B9, Canada.
J Hazard Mater. 2012 Oct 15;235-236:246-56. doi: 10.1016/j.jhazmat.2012.07.054. Epub 2012 Aug 4.
Mixed maghemite-magnetite has been used as adsorbent for Cr(VI) removal in this study. Results show that the adsorption capacity is enhanced with an increase in reaction temperature and decrease in free energy change. Thermodynamic study shows that Cr(VI) adsorption on the mixed maghemite and magnetite is endothermic in nature and is dependent on solution pH between 3 and 6. X-ray photoelectron spectroscopy (XPS) results demonstrate the theoretical multiplet peaks for iron and chromium adsorbed iron at the surface of the γ-Fe(2)O(3) and Fe(3)O(4) mixture. Theoretical multiplet analysis shows that during Cr adsorption, the amount of maghemite increases (from 70 to 89%). In magnetite spectra, the relative content of Fe(II) decreases from 8.2 to 3.6% indicating the reduction of magnetite in the mixture particles. In Raman spectroscopy studies, clear peaks of chromium on iron oxide were generated at 826 cm(-1), which could be attributed to chemical interactions between chromium compound and iron oxide. From the results of Raman and XPS studies, electrostatic attraction and oxidation-reduction between chromium and mixed maghemite-magnetite are postulated as mechanisms for the removal of Cr(VI) from aqueous solutions.
本研究采用磁赤铁矿-磁铁矿混合物作为吸附剂去除 Cr(VI)。结果表明,吸附容量随反应温度的升高和自由能变化的降低而增强。热力学研究表明,Cr(VI)在混合磁赤铁矿和磁铁矿上的吸附是吸热的,取决于溶液 pH 值在 3 到 6 之间。X 射线光电子能谱 (XPS) 结果表明,铁和铬的理论多重峰吸附在 γ-Fe(2)O(3)和 Fe(3)O(4)混合物表面的铁上。理论多重分析表明,在 Cr 吸附过程中,磁赤铁矿的含量增加(从 70%增加到 89%)。在磁铁矿光谱中,Fe(II)的相对含量从 8.2%下降到 3.6%,表明混合物颗粒中的磁铁矿还原。在拉曼光谱研究中,在 826 cm(-1)处生成了氧化铁上铬的清晰峰,这可归因于铬化合物与氧化铁之间的化学相互作用。根据拉曼和 XPS 研究的结果,提出了静电吸引和 Cr 与混合磁赤铁矿-磁铁矿之间的氧化还原作用作为从水溶液中去除 Cr(VI)的机制。