Manifestation of nitrogen interstitials in synthetic diamonds obtained using a temperature gradient technique (Fe–Ni–C system)
- Autores: Babich Y.V.1, Feigelson B.N.2, Chepurov A.I.1
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Afiliações:
- Institute of Geology and Mineralogy, Siberian Branch
- US Naval Research Laboratory
- Edição: Volume 54, Nº 10 (2016)
- Páginas: 922-927
- Seção: Article
- URL: https://journals.rcsi.science/0016-7029/article/view/155323
- DOI: https://doi.org/10.1134/S0016702916100025
- ID: 155323
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Resumo
The IR-peak 1450 cm–1 (H1a-center) associated with nitrogen interstitials have been studied in nitrogen-bearing diamonds synthesized at high P-T parameters in the Fe–Ni–C system. FTIR study shows that manifestation of this nitrogen form is restricted to the regions of active transformation of C-defects into A-defects, which confirms the connection of its formation with C => A aggregation process. An examination of the dependence of the 1450 cm–1 peak on the degree of nitrogen aggregation indicates that H1a-centers are not only formed during C/A aggregation but also disappear simultaneously with the end of C => A transformation. Established facts suggest direct involving of nitrogen as interstitials in the C => A aggregation and serve as strong experimental argument in support of the “interstitial” mechanism of nitrogen migration during aggregation in diamonds containing transition metals.
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Sobre autores
Yu. Babich
Institute of Geology and Mineralogy, Siberian Branch
Autor responsável pela correspondência
Email: babich@igm.nsc.ru
Rússia, pr. Koptyuga 3, Novosibirsk, 630090
B. Feigelson
US Naval Research Laboratory
Email: babich@igm.nsc.ru
Estados Unidos da América, Washington DC, 20375
A. Chepurov
Institute of Geology and Mineralogy, Siberian Branch
Email: babich@igm.nsc.ru
Rússia, pr. Koptyuga 3, Novosibirsk, 630090
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