高温低压处理黑色钻石的宝石学及光谱学特征

Gemmological and Spectroscopic Characteristics of Black Diamond Treated at High Temperature and Low Pressure

  • 摘要: 石墨作为钻石的同素异形体,在特定温度压力条件下二者可以发生相互转化,目前市场常见的处理黑色钻石就是利用此原理,通过在高温低压条件下促使钻石表层及内部产生大量石墨包裹体,大量微晶石墨使其为黑色。有效区分天然石墨包裹体致色的黑色钻石和高温低压处理的黑色钻石一直是实验室检测的难点。为此,本研究选取3粒天然褐色钻石样品进行高温低压处理实验,并收集10粒高温低压处理黑色钻石成品,分别从微晶石墨的形态与分布特征、拉曼光谱及钻石的发光图像、光致发光光谱共4个方面,对高温低压处理黑色钻石的宝石学及光谱学特征进行分析。结果显示,高温低压处理所产生的微晶石墨主要分布于处理钻石样品开放大裂隙面上,无石墨特定形态,局部表层可见大量密集排列的微晶石墨,原有白色云状包裹体体积增大并变为黑色点状物;微晶石墨包裹体的拉曼光谱主要表现为位于1 590 cm-1附近宽带,由于石墨D带的存在致使钻石的拉曼本征峰发生变形,证明高温低压处理产生的微晶石墨的有序度低于天然钻石中的石墨;高温低压处理黑色钻石样品的发光图像特征主要表现为整体较暗的蓝色荧光,裂隙处呈荧光惰性,裂隙附近可见由H3缺陷导致的绿色发光,部分样品可见“荧光笼”现象。光致发光光谱缺失以600、650 nm为中心的发光宽带及GR1缺陷,并出现强度不等的H2缺陷。微晶石墨包裹体特征及其光谱特征可以作为鉴定高温低压处理黑色钻石的主要依据。

     

    Abstract: Graphite, as an allotrope of diamond, can undergo mutual transformation with diamond under specific temperature and pressure conditions. Currently, a common treatment for black diamonds in the market utilizes this principle. Graphite inclusions are generated within and on the surface of the diamond under high temperature and low pressure (HTLP) conditions and the abundance of microcrystalline graphite renders the diamond black. Effectively distinguishing natural black diamonds coloured by graphite inclusions from HTLP-treated black diamonds has always been a challenge in laboratory testing.To address this, this study selected 3 natural brown diamond samples for HTLP treatment experiments and 10 HTLP-treated black diamonds. The gemmological and spectroscopic characteristics of the HTLP-treated black diamond samples were analyzed from 4 aspects: the morphology and distribution features of microcrystalline graphite, Raman spectroscopy, diamond luminescence imaging, and photoluminescence (PL) spectroscopy.The results show that the microcrystalline graphite produced by HTLP treatment is primarily distributed on the open fracture surfaces of the treated diamond samples, lacking a specific graphite morphology. Dense arrangements of microcrystalline graphite can be observed on local surface, while pre-existing white cloud-like inclusions expand in volume and turn into black speckles. The Raman spectra of the microcrystalline graphite inclusions mainly exhibit a broad band centered near 1 590 cm-1. Due to the presence of the graphite D-band, the intrinsic Raman peak of diamond becomes distorted, indicating that the microcrystalline graphite produced by HTLP treatment has a lower degree of ordering than natural graphite in diamonds.The luminescence imaging characteristics of the treated black diamond samples primarily manifest as an overall dark blue fluorescence; fractures exhibit fluorescence inertness. Green luminescence caused by H3 defect can be observed near the fractures, and some samples exhibit a "fluorescence cage" phenomenon. The PL spectra lack the broad emission bands centered at 600 nm and 650 nm, as well as the GR1 defect, while displaying H2 defect at varying intensities.The characteristics of microcrystalline graphite inclusions and their spectroscopic features in HTLP-treated black diamonds can serve as key indicators for their identification.

     

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