文摘
A stoichiometric nanosized Mn鈥揊e spinel (Fe2.2Mn0.8O4) was synthesized using a coprecipitation method. After the thermal treatment at 400 掳C under air, chemical heterogeneity deriving from the oxidation kinetic difference between Fe2+ and Mn2+/Mn3+ was observed in (Fe2.2Mn0.8)1-未O4. XPS and TEM analyses both pointed a Mn enrichment (especially Mn4+ cation) on the particle鈥檚 surface. Furthermore, the percent of cation vacancy on the surface increased obviously due to the enrichment of Mn4+ cation on the surface. As a result, the capacity of (Fe2.2Mn0.8)1-未O4-400 for elemental mercury capture was generally much better than those of MnOx/纬-Fe2O3, (Fe2.2Mn0.8)1-未O4-200 and Fe2.2Mn0.8O4. Furthermore, the saturation magnetization of (Fe2.2Mn0.8)1-未O4 obviously increased after the thermal treatment under air at 400 掳C, which made it easier to separate the sorbent and adsorbed mercury from the fly ash for recycling, regeneration, and safe disposal of the adsorbed mercury. Therefore, (Fe2.2Mn0.8)1-未O4-400 may be a promising sorbent for elemental mercury capture.