Magnetic hyperfine field distribution in pyrrhotites from Mössbauer spectroscopy

E. Reguera Ruiz; V. I. Nikolaev; V. S. Rusakov

doi:10.1007/BF02165896

Magnetic hyperfine field distribution in pyrrhotites from Mössbauer spectroscopy

E. Reguera Ruiz, V. I. Nikolaev, V. S. Rusakov

Producción científica: Contribución a una revista › Artículo › revisión exhaustiva

Resumen

Mössbauer spectra from intermediate pyrrhotite (Fe_1-xS) samples were interpreted according to their hyperfine magnetic field distribution functions at the Fe nuclei in these sulfides. Seven non-equivalent Mössbauer sites for Fe were distinguished by their peak positions in the distribution functions obtained.

Idioma original	Inglés
Páginas (desde-hasta)	423-429
Número de páginas	7
Publicación	Journal of Radioanalytical and Nuclear Chemistry Letters
Volumen	153
N.º	6
DOI	https://doi.org/10.1007/BF02165896
Estado	Publicada - abr. 1991
Publicado de forma externa	Sí

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@article{e8365e6be8f24810950f70517e795165,

title = "Magnetic hyperfine field distribution in pyrrhotites from M{\"o}ssbauer spectroscopy",

abstract = "M{\"o}ssbauer spectra from intermediate pyrrhotite (Fe1-xS) samples were interpreted according to their hyperfine magnetic field distribution functions at the Fe nuclei in these sulfides. Seven non-equivalent M{\"o}ssbauer sites for Fe were distinguished by their peak positions in the distribution functions obtained.",

author = "Ruiz, {E. Reguera} and Nikolaev, {V. I.} and Rusakov, {V. S.}",

year = "1991",

month = apr,

doi = "10.1007/BF02165896",

language = "Ingl{\'e}s",

volume = "153",

pages = "423--429",

journal = "Journal of Radioanalytical and Nuclear Chemistry Letters",

issn = "0236-5731",

number = "6",

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TY - JOUR

T1 - Magnetic hyperfine field distribution in pyrrhotites from Mössbauer spectroscopy

AU - Ruiz, E. Reguera

AU - Nikolaev, V. I.

AU - Rusakov, V. S.

PY - 1991/4

Y1 - 1991/4

N2 - Mössbauer spectra from intermediate pyrrhotite (Fe1-xS) samples were interpreted according to their hyperfine magnetic field distribution functions at the Fe nuclei in these sulfides. Seven non-equivalent Mössbauer sites for Fe were distinguished by their peak positions in the distribution functions obtained.

AB - Mössbauer spectra from intermediate pyrrhotite (Fe1-xS) samples were interpreted according to their hyperfine magnetic field distribution functions at the Fe nuclei in these sulfides. Seven non-equivalent Mössbauer sites for Fe were distinguished by their peak positions in the distribution functions obtained.

UR - http://www.scopus.com/inward/record.url?scp=0025855764&partnerID=8YFLogxK

U2 - 10.1007/BF02165896

DO - 10.1007/BF02165896

M3 - Artículo

SN - 0236-5731

VL - 153

SP - 423

EP - 429

JO - Journal of Radioanalytical and Nuclear Chemistry Letters

JF - Journal of Radioanalytical and Nuclear Chemistry Letters

IS - 6

ER -

Magnetic hyperfine field distribution in pyrrhotites from Mössbauer spectroscopy

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