Abstract

In this paper, the study of phase transition of tetragonal L 4-8 graphene into base-centered orthorhombic LA7 diamond polymorph is carried out using the density functional theory method. Analysis of the possible formation methods of LA7 phase showed that its structure can be obtained as a result of strong uniaxial compression of tetragonal graphite with packing of AB at a pressure of 42,5 GPa. The pressure at which LA7 phase can be synthesized is the lowest in comparison with the pressures at which other diamond polymorphs can be obtained. The calculations also showed that the process of this structural transformation should be accompanied by energy release of 0,52 eV/atom. The polymorphic modification of the diamond can stably exist under normal conditions, since the potential barrier separating states corresponding to graphite L 4-8 and LA7 phase is 0,34 eV/atom. The theoretical X-ray diffraction patterns of the "graphite L 4-8 – LA7" phase transition were calculated for the experimental identification of LA7 phase. The calculated powder X-ray diffraction pattern of the orthorhombic polymorph of diamond differs greatly from the X-ray diffraction patterns of graphite or cubic and hexagonal diamond polytypes.

Highlights

  • Введение Углеродные материалы с алмазоподобной структурой должны обладать высокими механическими характеристиками, так как они состоят из углеродных атомов в состояниях sp3гибридизации, связанных прочными ковалентными связями, и имеют трехмерную жесткосвязанную структуру [1,2]

  • Analysis of the possible formation methods of LA7 phase showed that its structure can be obtained as a result of strong uniaxial compression of tetragonal graphite with packing of AB at a pressure of 42,5 GPa

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Summary

Introduction

Введение Углеродные материалы с алмазоподобной структурой должны обладать высокими механическими характеристиками, так как они состоят из углеродных атомов в состояниях sp3гибридизации, связанных прочными ковалентными связями, и имеют трехмерную жесткосвязанную структуру [1,2]. В данной работе выполнены расчеты фазового превращения тетрагонального графита L4-8 в полиморфную разновидность алмаза LA7. Структура гексагонального политипа алмаза может быть сформирована при сильном сжатии P6/mmm графита L6 по оси [001].

Results
Conclusion

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