Evidence for valence fluctuation of Fe in Sr2FeMoO6-w double perovskite

J. Lindén; T. Yamamoto; M. Karppinen; H. Yamauchi; T. Pietari

doi:10.1063/1.126518

Evidence for valence fluctuation of Fe in Sr₂FeMoO_6-w double perovskite

J. Lindén, T. Yamamoto, M. Karppinen, H. Yamauchi^*, T. Pietari

^*Tämän työn vastaava kirjoittaja

Fysiikka

Tutkimustuotos: Lehtiartikkeli › Artikkeli › Tieteellinen › vertaisarvioitu

193 Sitaatiot (Scopus)

Abstrakti

In this letter evidence for the formation of a valence-fluctuation state of iron, formally denoted as Fe^2.5+, is presented. The system under study is the Sr₂FeMoO_6-w double perovskite, known for exhibiting a very large magnetoresistance. Samples of Sr₂FeMoO_6-w were synthesized by means of an encapsulation technique utilizing an Fe getter technique and characterized by ⁵⁷Fe Mössbauer spectroscopy. From 5 K to room temperature the Mössbauer spectrum is dominated by a component with hyperfine parameter values between those expected for high-spin Fe³⁺ and high-spin Fe²⁺.

Alkuperäiskieli	Englanti
Sivut	2925-2927
Sivumäärä	3
Julkaisu	Applied Physics Letters
Vuosikerta	76
Numero	20
DOI - pysyväislinkit	https://doi.org/10.1063/1.126518
Tila	Julkaistu - 15 toukok. 2000
OKM-julkaisutyyppi	A1 Julkaistu artikkeli, soviteltu

Pääsy asiakirjaan

10.1063/1.126518

Muut tiedostot ja linkit

Link to publication in Scopus

Viittausmuodot

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title = "Evidence for valence fluctuation of Fe in Sr2FeMoO6-w double perovskite",

abstract = "In this letter evidence for the formation of a valence-fluctuation state of iron, formally denoted as Fe2.5+, is presented. The system under study is the Sr2FeMoO6-w double perovskite, known for exhibiting a very large magnetoresistance. Samples of Sr2FeMoO6-w were synthesized by means of an encapsulation technique utilizing an Fe getter technique and characterized by 57Fe M{\"o}ssbauer spectroscopy. From 5 K to room temperature the M{\"o}ssbauer spectrum is dominated by a component with hyperfine parameter values between those expected for high-spin Fe3+ and high-spin Fe2+.",

author = "J. Lind{\'e}n and T. Yamamoto and M. Karppinen and H. Yamauchi and T. Pietari",

year = "2000",

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doi = "10.1063/1.126518",

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T1 - Evidence for valence fluctuation of Fe in Sr2FeMoO6-w double perovskite

AU - Lindén, J.

AU - Yamamoto, T.

AU - Karppinen, M.

AU - Yamauchi, H.

AU - Pietari, T.

PY - 2000/5/15

Y1 - 2000/5/15

N2 - In this letter evidence for the formation of a valence-fluctuation state of iron, formally denoted as Fe2.5+, is presented. The system under study is the Sr2FeMoO6-w double perovskite, known for exhibiting a very large magnetoresistance. Samples of Sr2FeMoO6-w were synthesized by means of an encapsulation technique utilizing an Fe getter technique and characterized by 57Fe Mössbauer spectroscopy. From 5 K to room temperature the Mössbauer spectrum is dominated by a component with hyperfine parameter values between those expected for high-spin Fe3+ and high-spin Fe2+.

AB - In this letter evidence for the formation of a valence-fluctuation state of iron, formally denoted as Fe2.5+, is presented. The system under study is the Sr2FeMoO6-w double perovskite, known for exhibiting a very large magnetoresistance. Samples of Sr2FeMoO6-w were synthesized by means of an encapsulation technique utilizing an Fe getter technique and characterized by 57Fe Mössbauer spectroscopy. From 5 K to room temperature the Mössbauer spectrum is dominated by a component with hyperfine parameter values between those expected for high-spin Fe3+ and high-spin Fe2+.

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DO - 10.1063/1.126518

M3 - Article

AN - SCOPUS:0011016819

SN - 0003-6951

VL - 76

SP - 2925

EP - 2927

JO - Applied Physics Letters

JF - Applied Physics Letters

IS - 20

ER -