Abstrac'/> LPHT annealing of brown-to-yellow type Ia diamonds
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LPHT annealing of brown-to-yellow type Ia diamonds

机译:棕色至黄色IA钻石的LPHT退火

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Abstract Low-pressure, high-temperature (LPHT) annealing of yellow-to-brown type Ia natural diamonds was performed to monitor its effects on optical centers within diamond, changes in the observed color, and to assess the process's viability as a commercial gem treatment. With LPHT annealing only, the mostly brown diamonds showed a shift towards yellow coloration; Vis-NIR absorption spectra showed this change was due to a modest increase in H3 intensity. Even at long annealing times (24h at 1800°C) or annealing at high temperatures (2000°C for five minutes), the diamonds did not significantly lose brown coloration. LPHT annealing showed itself as an ineffective means to break apart the vacancy clusters causing the brown color or causing nitrogen disaggregation, which resulted in only a small H3 generation. With LPHT annealing, “amber centers”—a group of several independent bands in the IR between 4200 and 4000cm?1 that disappear with HPHT annealing—were seen to anneal out gradually at various temperatures from 1700 to 2000°C. In contrast, high-pressure, high-temperature (HPHT) annealing effectively removes brown color at similar time/temperature conditions. Without the high stabilizing pressure provided by HPHT annealing techniques, the LPHT annealing showed pronounced damage on inclusions and dramatic surface etching. In subsequent experiments, LPHT annealing was used as a follow-up to laboratory irradiation. The irradiation-related vacancies created greater concentrations of H3 and the vacancy-assisted disaggregation of nitrogen created donors which led to a high concentration of H2 centers. This combination of defects resulted in a pronounced and favorable shift towards saleable yellow colors due to an increase in H3 and a dramatic increase in the H2 center, which led to the suppression of the remaining brownish component. The annealing characteristics for many centers detected by Vis-NIR absorption spectroscopy, FTIR absorption spectroscopy, and photoluminescence spectroscopy were chronicled throughout the study and compared with other LPHT annealing studies and HPHT annealing experiments. Graphical abstract Display Omitted Highlights ? Detailed study of the effects of low-pressure, high-temperature (LPHT) annealing on type Ia
机译:<![cdata [ Abstract 低压,高温(LPHT)退火的黄色棕色型IA天然钻石,以监测其对光学中心的影响在钻石中,观察颜色的变化,并评估过程作为商业宝石治疗的可行性。 只有lpht退火,大多数棕色钻石显示出黄色着色的转变; Vis-nir吸收光谱显示出这种变化是由于H3强度的适度增加。即使在长退火时期(24 h,在1800 °C)或在高温下退火(2000 °C五分钟),钻石没有显着丢失棕色着色。 LPHT退火表明,作为一种不可取的手段,可以分解导致棕色或导致氮素分解的空位簇分解,这仅导致小的H3代。 使用LPHT退火,”琥珀色中心“-A在IR中的几个独立频段,在IR之间的4200和4000之间 CM 1 用hpht退火消失 - 被视为从1700至2000的各种温度下逐渐退火 °C。 相反,高压,高温(HPHT)退火有效地除去棕色,类似时间/温度条件。如果没有HPHT退火技术提供的高稳定压力,则LPHT退火显示出夹杂物和戏剧性表面蚀刻的明显损坏。 随后的实验,LPHT退火用作实验室辐射的后续行动。与辐照相关的空位产生了更高的H3浓度,并且氮产生的氮的空位辅助分解,其导致高浓度的H2中心。由于H3的增加和H2中心的增加,这种缺陷的这种缺陷的组合导致了可销售的黄色颜色的转变,这导致抑制剩余的褐色成分。 < CE:简单 - 段ID =“SP0080”视图=“全部”>在整个研究中编年反红外测量光谱,FTIR吸收光谱和光致发光光谱检测的许多中心的退火特性,并与其他LPHT退火研究相比HPHT退火实验。 图形摘要 亮点 详细研究低压,高-Temperature(LPHT)IA型退火

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