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再次访问的阿达曼坦土地

Pedro H Antunes Silva1, Amir L Perlin1, Cleverson J F de Oliveira2

  • 1Instituto de Química, Universidade Federal do Rio de Janeiro, Av. Athos da Silveira Ramos, 149, CT A-622, Cid. Univ., Rio de Janeiro, RJ 21941-909, Brazil.

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像阿达曼坦一样,钻石氧化物是稳定的石油成分. 这项研究表明,虽然阿达曼坦是稳定的,但其碳酸并不是最稳定的,这表明1-甲基六胺和钻石形状形成之间存在联系.

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科学领域:

  • 地质化学 地质化学
  • 有机化学 有机化学
  • 石油科学 石油科学 石油科学

背景情况:

  • 钻石类是石油中发现的稳定,形的碳化合物.
  • 它们的地质稳定性使得它们成为有价值的标记物,但形成途径尚不清楚.
  • 与传统生物标志物相比,有限的知识阻碍了更广泛的应用.

研究的目的:

  • 为了研究阿达曼坦的形成路径,这是最简单的钻石.
  • 探索由异构碳化合物产生的碳酸化机制.
  • 评估阿达曼坦及其与异构体相对的碳酸的热力学稳定性.

主要方法:

  • 使用M06-2X/cc-pVTZ理论水平的计算化学.
  • 评估了阿达曼坦 (C10H16) 和1-阿达曼 (C10H15+) 异构体的热力学稳定性.
  • 亚达曼坦异构体和1-亚达曼离子异构体的比较稳定性.

主要成果:

  • 亚曼坦被证实是最稳定的C10H16异构体.
  • 1-阿达曼基离子不是最稳定的C10H15+物种.
  • 最稳定的碳酸盐是具有1-甲基六氨基环系统的类物种.

结论:

  • 具有1-甲基六胺结构的碳化合物可能在地化学上与钻石形状形成有关.
  • 这些碳化合物的比例可能是重要的地化学指标.
  • 了解这些路径可以提高钻石体作为地质标记的应用.