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HPHT synthesis of diamond with high nitrogen content from an Fe_3N-C system

机译:Fe_3N-C系统的HPHT合成高氮含量的金刚石

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摘要

The capability of iron ntiride, Fe_3N for converting graphite to diamond was explored at P=7 GPa and T=1550-1850 deg C in experiments with a duration of 20 h. It was established that depending on the synthesis temperature the iron nitride melt provides conditions for crystallisation of diamond and/or graphite, with the minimal temperature for spontaneous diamond nucleation being approximately 1700 deg C. Based on the results obtained it was argued that the iron nitride acts as the solvent-catalyst for diamond formation. The crystallised diamonds were found to contain nitrogen in concentration up to approximately 3300 ppm, which depending on the synthesis temperature was present in either the A form orboth A and C forms. Absorption peaks caused by hydrogen-related defects were observed in IR spectra of all diamonds examined. For the 3107 cm~(-1) line a tendency to increase in intensity with increasing the nitrogen content was found. The well-known blue band-A, N3, H3 and 2.156 eV systems as well as a band with zero-phonon energy at 1.78 eV were observed in cathodoluminescence.
机译:在持续20小时的实验中,在P = 7 GPa和T = 1550-1850℃的条件下,研究了氮化铁Fe_3N将石墨转化为金刚石的能力。已经确定,取决于合成温度,氮化铁熔体为金刚石和/或石墨的结晶提供条件,自发金刚石成核的最低温度约为1700℃。基于所获得的结果,认为氮化铁充当金刚石形成的溶剂催化剂。发现结晶的金刚石含有浓度高达约3300ppm的氮,其取决于合成温度以A形式或A和C形式存在。在所有检查的钻石的红外光谱中均观察到由氢相关缺陷引起的吸收峰。对于3107 cm〜(-1)线,发现强度随氮含量的增加而增加。在阴极发光中观察到了著名的蓝带A,N3,H3和2.156 eV系统,以及在1.78 eV具有零声子能量的谱带。

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