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A model of HPHT color enhancement mechanism in natural gray diamonds

机译:天然灰色钻石中HPHT增色机理的模型

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摘要

In the present paper HPHT-processing of natural gray graphite containing diamonds is studied and a new model of the color enhancement mechanism is proposed. It is proposed that there occurs a polymorphous transformation of graphite inclusion into diamond during HPHT-processing. During this transformation hydrogen, the content of which depends to a great extent on the number of graphite inclusions, is transferred from graphite to diamond getting localized on the nearest structural defects with uncopensated negative charges. In the optical spectra this ia accompanied by an anomalous increase in the intensity of the hydrogen-related lines in the IR spectrum. It has been observed that the intensity increases in the 2.988 eV line attributed to N3 centers after HPHT-processing at an unusually low temperature of 1800 deg C. In natural brown diamonds the intensity increase of the 2.988 eV line takes place at higher HPHT temperatures (over 200 deg C).
机译:在本文中,研究了高温高压处理含钻石的天然灰色石墨的方法,并提出了一种新的增色机理模型。有人提出在高温高压处理过程中,石墨夹杂物会发生多态转变成金刚石。在这种转变过程中,氢的含量在很大程度上取决于石墨夹杂物的数量,氢从石墨转移到金刚石上,并定位在最接近的结构缺陷上,这些缺陷带有未打开的负电荷。在光谱中,这伴随着红外光谱中与氢有关的线的强度异常增加。据观察,在异常高温1800摄氏度下进行HPHT处理后,归因于N3中心的2.988 eV线的强度增加。在天然棕色钻石中,2.988 eV线的强度增加发生在更高的HPHT温度下(超过200摄氏度)。

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