4.6 Article

Diamond powders synthesized at high pressure and high temperature from graphite with nickel in the presence of aluminum. Applicability of methods for analyzing nitrogen concentration in diamonds

Journal

JOURNAL OF SOLID STATE CHEMISTRY
Volume 307, Issue -, Pages -

Publisher

ACADEMIC PRESS INC ELSEVIER SCIENCE
DOI: 10.1016/j.jssc.2021.122804

Keywords

High-pressure high-temperature synthesis; Nitrogen content in diamond powders; Nitrogen getter; FTIR EPR and Raman spectroscopies; Spontaneous nucleation

Funding

  1. Ioffe Institute [0040-2019-0013]

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This study synthesized two samples of microcrystalline diamond powders under high pressure and temperature conditions, calculated the nitrogen content in diamond crystals using different methods, and found that some commonly used equations may give overestimated values; Additionally, the addition of aluminum powder can reduce spontaneous nucleation, leading to a change in crystal size distribution.
Two samples of microcrystalline diamond powders (<200 mu m) were synthesized with high growth rates at high pressure (5 GPa) and temperature (1650 degrees C) in a graphite-nickel medium (reference sample #D) and in the same mixture with the addition of aluminum powder (#DAl). Commercial diamond powder SDB1100 was used as a reference. The content of nitrogen in various forms (substitutional, charged substitutional, pairs) in diamond crystals was calculated from the FTIR, EPR, and Raman scattering data using different approaches. It is shown that some equations widely used to determine the concentration of nitrogen in diamond crystals give overestimated values and should be used with caution. The size fractionation of the synthesized diamond powders makes it possible to reveal the features of crystallization and the effect of aluminum on the growth patterns. The nitrogen concentration in sample #DAl is 100-190 ppm, which is about 2-4 times less than in sample #D. Aluminum significantly reduces spontaneous nucleation, which leads to a change in the crystal size distribution with the predominance of large crystals.

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