A Revisited Mechanism of the Graphite-to-Diamond Transition at High Temperature

被引:70
作者
Zhu, Sheng-cai [1 ,2 ]
Yan, Xiao-zhi [3 ,4 ]
Liu, Jin [5 ]
Oganov, Artem R. [6 ]
Zhu, Qiang [1 ]
机构
[1] Univ Nevada, Dept Phys & Astron, Las Vegas, NV 89154 USA
[2] Sun Yat Sen Univ, Sch Mat, Guangzhou 510275, Peoples R China
[3] Southern Univ Sci & Technol, Acad Adv Interdisciplinary Studies, Shenzhen 518055, Peoples R China
[4] Southern Univ Sci & Technol, Dept Phys, Shenzhen 518055, Peoples R China
[5] Jingchu Univ Technol, Sch Mech Engn, Jingmen 44800, Peoples R China
[6] Skolkovo Inst Sci & Technol, 3 Nobel St, Moscow 143026, Russia
关键词
SURFACE WALKING METHOD; POLYCRYSTALLINE DIAMOND; HIGH-PRESSURE; TOTAL-ENERGY; DIRECT CONVERSION; TRANSFORMATION; LONSDALEITE; NUCLEATION; ORIGIN; CARBON;
D O I
10.1016/j.matt.2020.05.013
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
The graphite-diamond transition, under high-pressure and high-temperature conditions, has been a central subject in physical science. However, its atomistic mechanism remains under debate. Employing large-scale molecular dynamics (MD) simulations, we report a mechanism whereby the diamond nuclei in the graphite matrix propagate in two preferred directions, among which the graphite [ 120] is about 2.5 times faster than [001]. Consequently, cubic diamond (CD) is the kinetically favorable product, while only a few hexagonal diamonds (HDs) can exist as the twins of CDs. The coherent interface of t-(100)gr//(11-1)cd + [010]gr//[1-10]cd observed in MD simulation was confirmed by our high-resolution transmission electron microscopy experiment. The proposed mechanism not only clarifies the role of HD in graphite-diamond transition but also yields atomistic insight into strengthening synthetic diamond via microstructure engineering.
引用
收藏
页码:864 / 878
页数:15
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