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首页> 外文期刊>Journal of Crystal Growth >Effect of fluid concentration on the formation of diamond in the CO_2-H_2O-graphite system under HP-HT conditions
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Effect of fluid concentration on the formation of diamond in the CO_2-H_2O-graphite system under HP-HT conditions

机译:HP-HT条件下流体浓度对CO_2-H_2O-石墨体系中金刚石形成的影响

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By changing the amount of fluid source to that of graphite by the way of loading both materials, the effect of fluid concentration on the formation of diamond was investigated at 7.7 Gpa and 1500 deg.C for 24 h in the system of graphite and CO_2-H_2O fluid, where anhydrous oxalic acid was used as a fluid source. In the samples where powders of oxalic acid and graphite were loaded separately into a platinum-sealed capsule, diamond yield was greatly affected by the fluid concentration. Namely, when the molar ratio of fluid to graphite was about 0.1, only a small amount of graphite of less than 20/100 was transformed into diamond, but the diamond yield increased to about 90/100 when the molar ratio of fluid increased to one. When powders of oxalic acid and graphite were mixed before being loaded, the transformation reaction became accelerated remarkably.
机译:通过加载两种材料的方式将流体源的量改为石墨,在石墨和CO_2-的体系中,在7.7 Gpa和1500℃下研究了流体浓度对金刚石形成的影响24 h。 H_2O流体,其中使用无水草酸作为流体源。在将草酸和石墨粉末分别装入铂密封胶囊中的样品中,钻石的收率受液体浓度的影响很大。即,当流体与石墨的摩尔比为约0.1时,只有少量小于20/100的石墨转化为金刚石,但是当流体的摩尔比增大为1时,金刚石产率提高到约90/100。 。草酸和石墨粉末在加料前混合时,转化反应显着加速。

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