Evidence of a cubic iron sub-lattice in t-CuFe2O4 demonstrated by X-ray Absorption Fine Structure

被引:41
作者
Caddeo, Francesco [1 ,4 ]
Loche, Danilo [1 ]
Casula, Maria F. [2 ,3 ]
Corrias, Anna [1 ]
机构
[1] Univ Kent, Sch Phys Sci, Ingram Bldg, Canterbury CT2 7NH, Kent, England
[2] Univ Cagliari, INSTM, SS 554, Monserrato, CA, Italy
[3] Univ Cagliari, Dipartimento Sci Chim & Geol, SS 554, Monserrato, CA, Italy
[4] Martin Luther Univ Halle Wittenberg, ZIK SiLi Nano, Karl Freiherr von Fritsch Str 3, D-06120 Halle, Saale, Germany
基金
英国工程与自然科学研究理事会;
关键词
COPPER FERRITE SPINELS; CATION DISTRIBUTION; AUTO-COMBUSTION; THERMAL-DECOMPOSITION; MAGNETIC-PROPERTIES; PHASE-TRANSITION; NANOPARTICLES; CUFE2O4; TEMPERATURE; XANES;
D O I
10.1038/s41598-017-19045-8
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Copper ferrite, belonging to the wide and technologically relevant class of spinel ferrites, was grown in the form of t-CuFe2O4 nanocrystals within a porous matrix of silica in the form of either an aerogel or a xerogel, and compared to a bulk sample. Extended X-ray absorption fine structure (EXAFS) spectroscopy revealed the presence of two different sub-lattices within the crystal structure of t-CuFe2O4, one tetragonal and one cubic, defined by the Cu2+ and Fe3+ ions respectively. Our investigation provides evidence that the Jahn-Teller distortion, which occurs on the Cu2+ ions located in octahedral sites, does not affect the coordination geometry of the Fe3+ ions, regardless of their location in octahedral or tetrahedral sites.
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页数:12
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