Formation and cation distribution in supported manganese ferrite nanoparticles: an X-ray absorption study

被引:74
作者
Carta, Daniela
Casula, Maria Francesca
Mountjoy, Gavin [2 ]
Corrias, Anna [1 ]
机构
[1] Univ Cagliari, Dipartimento Sci Chim, I-09042 Cagliari, Italy
[2] Univ Kent, Sch Phys Sci, Canterbury CT2 7NH, Kent, England
关键词
D O I
10.1039/b800359a
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
Extended X-ray absorption fine structure (EXAFS) and X-ray absorption near-edge structure (XANES) techniques at both Fe and Mn K-edges were used to investigate the formation of MnFe2O4 nanoparticles embedded in a silica aerogel matrix as a function of calcination temperature (at 450, 750 and 900 degrees C). Up to 450 degrees C, two separated highly-disordered phases of iron and manganese are present. With increasing the temperature (to 750 and 900 degrees C), the structure of aerogel nanoparticles becomes progressively similar to that of the spinel structure MnFe2O4 (jacobsite). Quantitative determination of cations distribution in the spinel structure shows that aerogels calcined at 750 and 900 degrees C have a degree of inversion i = 0.20. A pure jacobsite sample synthesised by co-precipitation and used as a reference compound shows a much higher degree of inversion (i = 0.70). The different distribution of iron and manganese cations in the octahedral and tetrahedral sites in pure jacobsite and in the aerogels can be ascribed to partial oxidation of Mn2+ to Mn3+ in pure jacobsite, confirmed by XANES analysis, probably due to the synthesis conditions.
引用
收藏
页码:3108 / 3117
页数:10
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