Mössbauer study on M1 and M2 sites of $ Fe^{2+} $ in natural hypersthene under dynamic crystal field potential approach
Abstract 57Fe Mössbauer spectra of hypersthene, a natural silicate mineral belonging to the orthopyroxene group, have been taken over the temperature range 77–292 K. At temperatures above 77 K, they show asymmetric quadrupole peaks. This asymmetry arises from the overlapping of two quadrupole double...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Sinha, T. P. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1993 |
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| Schlagwörter: |
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| Anmerkung: |
© J.C. Baltzer AG, Science Publishers 1993 |
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| Übergeordnetes Werk: |
Enthalten in: Hyperfine interactions - Baltzer Science Publishers, Baarn/Kluwer Academic Publishers, 1975, 77(1993), 1 vom: Dez., Seite 29-42 |
|---|---|
| Übergeordnetes Werk: |
volume:77 ; year:1993 ; number:1 ; month:12 ; pages:29-42 |
| Links: |
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| DOI / URN: |
10.1007/BF02320296 |
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OLC2076373659 |
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| 245 | 1 | 0 | |a Mössbauer study on M1 and M2 sites of $ Fe^{2+} $ in natural hypersthene under dynamic crystal field potential approach |
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| 520 | |a Abstract 57Fe Mössbauer spectra of hypersthene, a natural silicate mineral belonging to the orthopyroxene group, have been taken over the temperature range 77–292 K. At temperatures above 77 K, they show asymmetric quadrupole peaks. This asymmetry arises from the overlapping of two quadrupole doublets from $ Fe^{2+} $($ 3d^{6} $,5D) ions in two different sites (M1 and M2). The quadrupole splitting, isomer shift and their temperature dependence are appreciably different for $ Fe^{2+} $ ions in the two sites. The $ Fe^{2+} $ quadrupole splitting in the M1 site decreases linearly with temperature, which can be explained quite satisfactorily by using a very simple model of the orbit-lattice interaction. | ||
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10.1007/BF02320296 doi (DE-627)OLC2076373659 (DE-He213)BF02320296-p DE-627 ger DE-627 rakwb eng 530 VZ 33.00 bkl Sinha, T. P. verfasserin aut Mössbauer study on M1 and M2 sites of $ Fe^{2+} $ in natural hypersthene under dynamic crystal field potential approach 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © J.C. Baltzer AG, Science Publishers 1993 Abstract 57Fe Mössbauer spectra of hypersthene, a natural silicate mineral belonging to the orthopyroxene group, have been taken over the temperature range 77–292 K. At temperatures above 77 K, they show asymmetric quadrupole peaks. This asymmetry arises from the overlapping of two quadrupole doublets from $ Fe^{2+} $($ 3d^{6} $,5D) ions in two different sites (M1 and M2). The quadrupole splitting, isomer shift and their temperature dependence are appreciably different for $ Fe^{2+} $ ions in the two sites. The $ Fe^{2+} $ quadrupole splitting in the M1 site decreases linearly with temperature, which can be explained quite satisfactorily by using a very simple model of the orbit-lattice interaction. Thin Film Silicate Simple Model Isomer Shift Crystal Field Das, D. aut Bhattacharya, M. aut Enthalten in Hyperfine interactions Baltzer Science Publishers, Baarn/Kluwer Academic Publishers, 1975 77(1993), 1 vom: Dez., Seite 29-42 (DE-627)129438685 (DE-600)194471-X (DE-576)014809028 0304-3843 nnns volume:77 year:1993 number:1 month:12 pages:29-42 https://doi.org/10.1007/BF02320296 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY GBV_ILN_20 GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_2279 GBV_ILN_4012 GBV_ILN_4046 33.00 VZ AR 77 1993 1 12 29-42 |
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10.1007/BF02320296 doi (DE-627)OLC2076373659 (DE-He213)BF02320296-p DE-627 ger DE-627 rakwb eng 530 VZ 33.00 bkl Sinha, T. P. verfasserin aut Mössbauer study on M1 and M2 sites of $ Fe^{2+} $ in natural hypersthene under dynamic crystal field potential approach 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © J.C. Baltzer AG, Science Publishers 1993 Abstract 57Fe Mössbauer spectra of hypersthene, a natural silicate mineral belonging to the orthopyroxene group, have been taken over the temperature range 77–292 K. At temperatures above 77 K, they show asymmetric quadrupole peaks. This asymmetry arises from the overlapping of two quadrupole doublets from $ Fe^{2+} $($ 3d^{6} $,5D) ions in two different sites (M1 and M2). The quadrupole splitting, isomer shift and their temperature dependence are appreciably different for $ Fe^{2+} $ ions in the two sites. The $ Fe^{2+} $ quadrupole splitting in the M1 site decreases linearly with temperature, which can be explained quite satisfactorily by using a very simple model of the orbit-lattice interaction. Thin Film Silicate Simple Model Isomer Shift Crystal Field Das, D. aut Bhattacharya, M. aut Enthalten in Hyperfine interactions Baltzer Science Publishers, Baarn/Kluwer Academic Publishers, 1975 77(1993), 1 vom: Dez., Seite 29-42 (DE-627)129438685 (DE-600)194471-X (DE-576)014809028 0304-3843 nnns volume:77 year:1993 number:1 month:12 pages:29-42 https://doi.org/10.1007/BF02320296 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY GBV_ILN_20 GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_2279 GBV_ILN_4012 GBV_ILN_4046 33.00 VZ AR 77 1993 1 12 29-42 |
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10.1007/BF02320296 doi (DE-627)OLC2076373659 (DE-He213)BF02320296-p DE-627 ger DE-627 rakwb eng 530 VZ 33.00 bkl Sinha, T. P. verfasserin aut Mössbauer study on M1 and M2 sites of $ Fe^{2+} $ in natural hypersthene under dynamic crystal field potential approach 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © J.C. Baltzer AG, Science Publishers 1993 Abstract 57Fe Mössbauer spectra of hypersthene, a natural silicate mineral belonging to the orthopyroxene group, have been taken over the temperature range 77–292 K. At temperatures above 77 K, they show asymmetric quadrupole peaks. This asymmetry arises from the overlapping of two quadrupole doublets from $ Fe^{2+} $($ 3d^{6} $,5D) ions in two different sites (M1 and M2). The quadrupole splitting, isomer shift and their temperature dependence are appreciably different for $ Fe^{2+} $ ions in the two sites. The $ Fe^{2+} $ quadrupole splitting in the M1 site decreases linearly with temperature, which can be explained quite satisfactorily by using a very simple model of the orbit-lattice interaction. Thin Film Silicate Simple Model Isomer Shift Crystal Field Das, D. aut Bhattacharya, M. aut Enthalten in Hyperfine interactions Baltzer Science Publishers, Baarn/Kluwer Academic Publishers, 1975 77(1993), 1 vom: Dez., Seite 29-42 (DE-627)129438685 (DE-600)194471-X (DE-576)014809028 0304-3843 nnns volume:77 year:1993 number:1 month:12 pages:29-42 https://doi.org/10.1007/BF02320296 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY GBV_ILN_20 GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_2279 GBV_ILN_4012 GBV_ILN_4046 33.00 VZ AR 77 1993 1 12 29-42 |
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10.1007/BF02320296 doi (DE-627)OLC2076373659 (DE-He213)BF02320296-p DE-627 ger DE-627 rakwb eng 530 VZ 33.00 bkl Sinha, T. P. verfasserin aut Mössbauer study on M1 and M2 sites of $ Fe^{2+} $ in natural hypersthene under dynamic crystal field potential approach 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © J.C. Baltzer AG, Science Publishers 1993 Abstract 57Fe Mössbauer spectra of hypersthene, a natural silicate mineral belonging to the orthopyroxene group, have been taken over the temperature range 77–292 K. At temperatures above 77 K, they show asymmetric quadrupole peaks. This asymmetry arises from the overlapping of two quadrupole doublets from $ Fe^{2+} $($ 3d^{6} $,5D) ions in two different sites (M1 and M2). The quadrupole splitting, isomer shift and their temperature dependence are appreciably different for $ Fe^{2+} $ ions in the two sites. The $ Fe^{2+} $ quadrupole splitting in the M1 site decreases linearly with temperature, which can be explained quite satisfactorily by using a very simple model of the orbit-lattice interaction. Thin Film Silicate Simple Model Isomer Shift Crystal Field Das, D. aut Bhattacharya, M. aut Enthalten in Hyperfine interactions Baltzer Science Publishers, Baarn/Kluwer Academic Publishers, 1975 77(1993), 1 vom: Dez., Seite 29-42 (DE-627)129438685 (DE-600)194471-X (DE-576)014809028 0304-3843 nnns volume:77 year:1993 number:1 month:12 pages:29-42 https://doi.org/10.1007/BF02320296 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY GBV_ILN_20 GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_2279 GBV_ILN_4012 GBV_ILN_4046 33.00 VZ AR 77 1993 1 12 29-42 |
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10.1007/BF02320296 doi (DE-627)OLC2076373659 (DE-He213)BF02320296-p DE-627 ger DE-627 rakwb eng 530 VZ 33.00 bkl Sinha, T. P. verfasserin aut Mössbauer study on M1 and M2 sites of $ Fe^{2+} $ in natural hypersthene under dynamic crystal field potential approach 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © J.C. Baltzer AG, Science Publishers 1993 Abstract 57Fe Mössbauer spectra of hypersthene, a natural silicate mineral belonging to the orthopyroxene group, have been taken over the temperature range 77–292 K. At temperatures above 77 K, they show asymmetric quadrupole peaks. This asymmetry arises from the overlapping of two quadrupole doublets from $ Fe^{2+} $($ 3d^{6} $,5D) ions in two different sites (M1 and M2). The quadrupole splitting, isomer shift and their temperature dependence are appreciably different for $ Fe^{2+} $ ions in the two sites. The $ Fe^{2+} $ quadrupole splitting in the M1 site decreases linearly with temperature, which can be explained quite satisfactorily by using a very simple model of the orbit-lattice interaction. Thin Film Silicate Simple Model Isomer Shift Crystal Field Das, D. aut Bhattacharya, M. aut Enthalten in Hyperfine interactions Baltzer Science Publishers, Baarn/Kluwer Academic Publishers, 1975 77(1993), 1 vom: Dez., Seite 29-42 (DE-627)129438685 (DE-600)194471-X (DE-576)014809028 0304-3843 nnns volume:77 year:1993 number:1 month:12 pages:29-42 https://doi.org/10.1007/BF02320296 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY GBV_ILN_20 GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_2279 GBV_ILN_4012 GBV_ILN_4046 33.00 VZ AR 77 1993 1 12 29-42 |
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mössbauer study on m1 and m2 sites of $ fe^{2+} $ in natural hypersthene under dynamic crystal field potential approach |
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Mössbauer study on M1 and M2 sites of $ Fe^{2+} $ in natural hypersthene under dynamic crystal field potential approach |
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Abstract 57Fe Mössbauer spectra of hypersthene, a natural silicate mineral belonging to the orthopyroxene group, have been taken over the temperature range 77–292 K. At temperatures above 77 K, they show asymmetric quadrupole peaks. This asymmetry arises from the overlapping of two quadrupole doublets from $ Fe^{2+} $($ 3d^{6} $,5D) ions in two different sites (M1 and M2). The quadrupole splitting, isomer shift and their temperature dependence are appreciably different for $ Fe^{2+} $ ions in the two sites. The $ Fe^{2+} $ quadrupole splitting in the M1 site decreases linearly with temperature, which can be explained quite satisfactorily by using a very simple model of the orbit-lattice interaction. © J.C. Baltzer AG, Science Publishers 1993 |
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Abstract 57Fe Mössbauer spectra of hypersthene, a natural silicate mineral belonging to the orthopyroxene group, have been taken over the temperature range 77–292 K. At temperatures above 77 K, they show asymmetric quadrupole peaks. This asymmetry arises from the overlapping of two quadrupole doublets from $ Fe^{2+} $($ 3d^{6} $,5D) ions in two different sites (M1 and M2). The quadrupole splitting, isomer shift and their temperature dependence are appreciably different for $ Fe^{2+} $ ions in the two sites. The $ Fe^{2+} $ quadrupole splitting in the M1 site decreases linearly with temperature, which can be explained quite satisfactorily by using a very simple model of the orbit-lattice interaction. © J.C. Baltzer AG, Science Publishers 1993 |
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Abstract 57Fe Mössbauer spectra of hypersthene, a natural silicate mineral belonging to the orthopyroxene group, have been taken over the temperature range 77–292 K. At temperatures above 77 K, they show asymmetric quadrupole peaks. This asymmetry arises from the overlapping of two quadrupole doublets from $ Fe^{2+} $($ 3d^{6} $,5D) ions in two different sites (M1 and M2). The quadrupole splitting, isomer shift and their temperature dependence are appreciably different for $ Fe^{2+} $ ions in the two sites. The $ Fe^{2+} $ quadrupole splitting in the M1 site decreases linearly with temperature, which can be explained quite satisfactorily by using a very simple model of the orbit-lattice interaction. © J.C. Baltzer AG, Science Publishers 1993 |
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Mössbauer study on M1 and M2 sites of $ Fe^{2+} $ in natural hypersthene under dynamic crystal field potential approach |
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https://doi.org/10.1007/BF02320296 |
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Das, D. Bhattacharya, M. |
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