Standard

Octahedral cation partitioning in Mg,Fe2+-olivine. Mössbauer spectroscopic study of synthetic (Mg0.5 Fe 2+0.5)2SiO4 (Fa50). / Morozov, Mikhail; Brinkmann, Christian; Grodzicki, Michael; Lottermoser, Werner; Tippelt, Gerold; Amthauer, Georg; Kroll, Herbert.

в: Hyperfine Interactions, Том 166, № 1-4, 11.2005, стр. 573-578.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Morozov, M, Brinkmann, C, Grodzicki, M, Lottermoser, W, Tippelt, G, Amthauer, G & Kroll, H 2005, 'Octahedral cation partitioning in Mg,Fe2+-olivine. Mössbauer spectroscopic study of synthetic (Mg0.5 Fe 2+0.5)2SiO4 (Fa50)', Hyperfine Interactions, Том. 166, № 1-4, стр. 573-578. https://doi.org/10.1007/s10751-006-9347-9

APA

Morozov, M., Brinkmann, C., Grodzicki, M., Lottermoser, W., Tippelt, G., Amthauer, G., & Kroll, H. (2005). Octahedral cation partitioning in Mg,Fe2+-olivine. Mössbauer spectroscopic study of synthetic (Mg0.5 Fe 2+0.5)2SiO4 (Fa50). Hyperfine Interactions, 166(1-4), 573-578. https://doi.org/10.1007/s10751-006-9347-9

Vancouver

Morozov M, Brinkmann C, Grodzicki M, Lottermoser W, Tippelt G, Amthauer G и пр. Octahedral cation partitioning in Mg,Fe2+-olivine. Mössbauer spectroscopic study of synthetic (Mg0.5 Fe 2+0.5)2SiO4 (Fa50). Hyperfine Interactions. 2005 Нояб.;166(1-4):573-578. https://doi.org/10.1007/s10751-006-9347-9

Author

Morozov, Mikhail ; Brinkmann, Christian ; Grodzicki, Michael ; Lottermoser, Werner ; Tippelt, Gerold ; Amthauer, Georg ; Kroll, Herbert. / Octahedral cation partitioning in Mg,Fe2+-olivine. Mössbauer spectroscopic study of synthetic (Mg0.5 Fe 2+0.5)2SiO4 (Fa50). в: Hyperfine Interactions. 2005 ; Том 166, № 1-4. стр. 573-578.

BibTeX

@article{6886d1d5064a4d10b8bac1feeb17acda,
title = "Octahedral cation partitioning in Mg,Fe2+-olivine. M{\"o}ssbauer spectroscopic study of synthetic (Mg0.5 Fe 2+0.5)2SiO4 (Fa50)",
abstract = "The high-temperature partitioning of Fe2+ and Mg between the two non-equivalent octahedral M1 and M2 sites in synthetic olivine (Fa 50) was studied by M{\"o}ssbauer spectroscopy. Powder samples have been equilibrated in annealing experiments performed under reducing oxygen fugacity at temperatures between 500 and 800°C followed by rapid quenching in order to prevent redistribution of cations. M-site ordering with Fe 2+ preferring M1, Mg preferring M2 sites increases continuously with rising equilibrium temperature. KD values increase from 1.21 at 500°C to 1.48 at 750°C. The results are consistent with both room temperature as well as in situ high temperature single crystal X-ray diffraction experiments of Heinemann et al. [8, 9].",
keywords = "Cation distribution, M{\"o}ssbauer spectroscopy, Olivine",
author = "Mikhail Morozov and Christian Brinkmann and Michael Grodzicki and Werner Lottermoser and Gerold Tippelt and Georg Amthauer and Herbert Kroll",
note = "Funding Information: Acknowledgments This work was partially supported by DFG and {\"O}AD grants, and also by the Russian Ministry of Education (grants PD02-1.5-361 and E02-2.0-58), Administration of St. Petersburg, Russia (grant PD03-1.5-55) and BRHE (grant Y1-G-15-01). Copyright: Copyright 2007 Elsevier B.V., All rights reserved.",
year = "2005",
month = nov,
doi = "10.1007/s10751-006-9347-9",
language = "English",
volume = "166",
pages = "573--578",
journal = "Hyperfine Interactions",
issn = "0304-3843",
publisher = "Springer Nature",
number = "1-4",

}

RIS

TY - JOUR

T1 - Octahedral cation partitioning in Mg,Fe2+-olivine. Mössbauer spectroscopic study of synthetic (Mg0.5 Fe 2+0.5)2SiO4 (Fa50)

AU - Morozov, Mikhail

AU - Brinkmann, Christian

AU - Grodzicki, Michael

AU - Lottermoser, Werner

AU - Tippelt, Gerold

AU - Amthauer, Georg

AU - Kroll, Herbert

N1 - Funding Information: Acknowledgments This work was partially supported by DFG and ÖAD grants, and also by the Russian Ministry of Education (grants PD02-1.5-361 and E02-2.0-58), Administration of St. Petersburg, Russia (grant PD03-1.5-55) and BRHE (grant Y1-G-15-01). Copyright: Copyright 2007 Elsevier B.V., All rights reserved.

PY - 2005/11

Y1 - 2005/11

N2 - The high-temperature partitioning of Fe2+ and Mg between the two non-equivalent octahedral M1 and M2 sites in synthetic olivine (Fa 50) was studied by Mössbauer spectroscopy. Powder samples have been equilibrated in annealing experiments performed under reducing oxygen fugacity at temperatures between 500 and 800°C followed by rapid quenching in order to prevent redistribution of cations. M-site ordering with Fe 2+ preferring M1, Mg preferring M2 sites increases continuously with rising equilibrium temperature. KD values increase from 1.21 at 500°C to 1.48 at 750°C. The results are consistent with both room temperature as well as in situ high temperature single crystal X-ray diffraction experiments of Heinemann et al. [8, 9].

AB - The high-temperature partitioning of Fe2+ and Mg between the two non-equivalent octahedral M1 and M2 sites in synthetic olivine (Fa 50) was studied by Mössbauer spectroscopy. Powder samples have been equilibrated in annealing experiments performed under reducing oxygen fugacity at temperatures between 500 and 800°C followed by rapid quenching in order to prevent redistribution of cations. M-site ordering with Fe 2+ preferring M1, Mg preferring M2 sites increases continuously with rising equilibrium temperature. KD values increase from 1.21 at 500°C to 1.48 at 750°C. The results are consistent with both room temperature as well as in situ high temperature single crystal X-ray diffraction experiments of Heinemann et al. [8, 9].

KW - Cation distribution

KW - Mössbauer spectroscopy

KW - Olivine

UR - http://www.scopus.com/inward/record.url?scp=33845790558&partnerID=8YFLogxK

U2 - 10.1007/s10751-006-9347-9

DO - 10.1007/s10751-006-9347-9

M3 - Article

AN - SCOPUS:33845790558

VL - 166

SP - 573

EP - 578

JO - Hyperfine Interactions

JF - Hyperfine Interactions

SN - 0304-3843

IS - 1-4

ER -

ID: 71137564