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J. Ramón Gancedo

Researcher at Spanish National Research Council

Publications -  7
Citations -  338

J. Ramón Gancedo is an academic researcher from Spanish National Research Council. The author has contributed to research in topics: Extended X-ray absorption fine structure & XANES. The author has an hindex of 6, co-authored 7 publications receiving 312 citations.

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Journal ArticleDOI

Cation distribution and magnetic structure of the ferrimagnetic spinel NiCo2O4

TL;DR: In this paper, the properties of the compound NiCo2O4 with spinel-related structure have been examined by means of magnetic measurements, neutron diffraction, X-ray absorption near edge structure (XANES) and extended Xray absorption fine structure (EXAFS), and the results suggest a delocalised electron distribution on the octahedral sites with average oxidation states of +3.5 and +2.5 for nickel and cobalt, respectively, and lead to a cation distribution for NiCo 2O4 of {Ni3+0.
Journal ArticleDOI

Synthesis and characterization of the reduction properties of cobalt-substituted lanthanum orthoferrites

TL;DR: In this article, the reduction process of LaFe1-xCoxO3 has been examined by Fe-57 Mossbauer spectroscopy and Fe K-edge, Co Kedge, and La L-III-edge XANES and EXAFS.
Journal ArticleDOI

Characterization of the Mn–Li ferrite system Li1−0.5xFe1.5x+1Mn1−xO4 (0.2 ≤x≤ 1)

TL;DR: In this paper, the spinel-related structure of the Mn-Li ferrite system was studied by means of X-ray diffraction, Mossbauer spectroscopy and Mn K- and Fe K-edge XANES/EXAFS.
Journal ArticleDOI

The oxidation states of titanium and niobium in compounds of composition SnxNbTiP3O12 (0 < x ⩽ 0.50) : an XPS study

TL;DR: In this paper, the oxidation states of titanium and niobium in compounds of composition Sn x NbTiP 3 O 12 (0 x ⩽ 0.50) have been examined by X-ray photoelectron spectroscopy.
Book ChapterDOI

57 Fe Mössbauer Spectroscopy Study of LaFe 1-x Co x O 3 (x=0 and 0.5) Formed by Mechanical Milling

TL;DR: In this paper, the reduction of LaFe0.5Co 0.5O3 in a reducing atmosphere leads to reduction of both Fe3+ and Co3+, their segregation from the oxide matrix, and the formation of an iron-cobalt alloy.