Manifestation of nitrogen interstitials in synthetic diamonds obtained using a temperature gradient technique (Fe–Ni–C system)


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Abstract

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.

About the authors

Yu. V. Babich

Institute of Geology and Mineralogy, Siberian Branch

Author for correspondence.
Email: babich@igm.nsc.ru
Russian Federation, pr. Koptyuga 3, Novosibirsk, 630090

B. N. Feigelson

US Naval Research Laboratory

Email: babich@igm.nsc.ru
United States, Washington DC, 20375

A. I. Chepurov

Institute of Geology and Mineralogy, Siberian Branch

Email: babich@igm.nsc.ru
Russian Federation, pr. Koptyuga 3, Novosibirsk, 630090

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