{"title":"Synthesis of Diamonds and Their Identification","authors":"U. D’Haenens-Johansson, J. E. Butler, A. Katrusha","doi":"10.2138/rmg.2022.88.13","DOIUrl":null,"url":null,"abstract":"Since 1797, when Tennant demonstrated that diamond consists solely of elemental carbon by comparing the volume of carbon dioxide formed by burning identical weights of charcoal and diamond (Tennant 1797), scientists have been trying to synthesize diamond by converting various carbon-containing substances. Several attempts followed, but it would take over 150 years of continued research before the first successful report of diamond growth was published by scientists at General Electric (Bundy et al. 1955). Diamond synthesis by Union Carbide in 1952 and Allmänna Svenska Elektriska Aktiebolaget (ASEA) in 1953 predate the work at General Electric, but were not reported until later (Liander and Lundblad 1960; Eversole 1962; Angus 2014). The most familiar carbon allotropes are the crystalline phases of graphite and diamond. The hexagonal form of graphite consists of sheets of sp2 hybridized carbon atoms in a hexagonal array, with each atom bonded to three equidistant nearest neighbor atoms. The layers are attracted to each other by weak van der Waals forces and may be arranged in a hexagonal, or rarely rhombohedral, stacking sequence. Meanwhile, the carbon orbitals in diamond are sp3 hybridized, with each atom covalently bonded to four nearest neighbors in a tetrahedral arrangement. The prevalent diamond structure is cubic, though the hexagonal lonsdaleite form also exists. Figure 1 illustrates the pressure and temperature (P, T) phase and transition diagram for pure carbon. Theoretically and experimentally determined conditional phase boundary lines separate the diamond and graphite stability fields. The high cohesive and activation energies associated with the different carbon phases mean that other metastable forms can occur under conditions at which they are not thermodynamically stable. For instance, diamond exists at room temperatures and pressures, whereas graphite can survive pressures well into the diamond stability field (Bundy 1980; Bundy et al. 1996).","PeriodicalId":439110,"journal":{"name":"Reviews in Mineralogy and Geochemistry","volume":"1 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2022-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"6","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Reviews in Mineralogy and Geochemistry","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.2138/rmg.2022.88.13","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 6
Abstract
Since 1797, when Tennant demonstrated that diamond consists solely of elemental carbon by comparing the volume of carbon dioxide formed by burning identical weights of charcoal and diamond (Tennant 1797), scientists have been trying to synthesize diamond by converting various carbon-containing substances. Several attempts followed, but it would take over 150 years of continued research before the first successful report of diamond growth was published by scientists at General Electric (Bundy et al. 1955). Diamond synthesis by Union Carbide in 1952 and Allmänna Svenska Elektriska Aktiebolaget (ASEA) in 1953 predate the work at General Electric, but were not reported until later (Liander and Lundblad 1960; Eversole 1962; Angus 2014). The most familiar carbon allotropes are the crystalline phases of graphite and diamond. The hexagonal form of graphite consists of sheets of sp2 hybridized carbon atoms in a hexagonal array, with each atom bonded to three equidistant nearest neighbor atoms. The layers are attracted to each other by weak van der Waals forces and may be arranged in a hexagonal, or rarely rhombohedral, stacking sequence. Meanwhile, the carbon orbitals in diamond are sp3 hybridized, with each atom covalently bonded to four nearest neighbors in a tetrahedral arrangement. The prevalent diamond structure is cubic, though the hexagonal lonsdaleite form also exists. Figure 1 illustrates the pressure and temperature (P, T) phase and transition diagram for pure carbon. Theoretically and experimentally determined conditional phase boundary lines separate the diamond and graphite stability fields. The high cohesive and activation energies associated with the different carbon phases mean that other metastable forms can occur under conditions at which they are not thermodynamically stable. For instance, diamond exists at room temperatures and pressures, whereas graphite can survive pressures well into the diamond stability field (Bundy 1980; Bundy et al. 1996).
1797年,坦南特通过比较燃烧相同重量的木炭和钻石所产生的二氧化碳的体积,证明了钻石仅由单质碳组成(坦南特1797年)。自那以后,科学家们一直试图通过转化各种含碳物质来合成钻石。随后进行了几次尝试,但通用电气的科学家们花了150多年的时间才发表了第一份成功的钻石生长报告(Bundy et al. 1955)。联合碳化物公司在1952年和Allmänna Svenska Elektriska Aktiebolaget (ASEA)在1953年的金刚石合成工作早于通用电气的工作,但直到后来才被报道(Liander and Lundblad 1960;Eversole 1962;安格斯2014年)。最常见的碳同素异形体是石墨和金刚石的结晶相。六角形石墨是由sp2杂化碳原子组成的六角形排列,每个原子与三个距离相等的近邻原子相连。这些层在弱范德华力的作用下相互吸引,可以排列成六角形堆叠序列,很少是菱形堆叠序列。同时,金刚石中的碳轨道是sp3杂化的,每个碳原子以四面体的形式与最近的四个碳原子共价键成键。普遍的钻石结构是立方的,虽然也存在六方的菱形结构。图1显示了纯碳的压力和温度(P, T)相和转变图。从理论上和实验上确定了金刚石和石墨稳定场的条件相边界线。与不同碳相相关的高内聚能和活化能意味着其他亚稳态形式可以在它们不热力学稳定的条件下发生。例如,金刚石存在于室温和室温压力下,而石墨可以在金刚石稳定场中很好地承受压力(Bundy 1980;邦迪等人,1996)。