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Comment on “Incipient plasticity of diamond during nanoindentation” by C. Xu, C. Liu and H. Wang, RSC Advances, 2017, 7, 36093

Saurav Goel *a and Alexander Stukowski b
aCranfield University, MK430AL, UK. E-mail: s.goel@cranfield.ac.uk
bDarmstadt University of Technology, Darmstadt, D-64287, Germany

Received 7th November 2017 , Accepted 24th January 2018

First published on 31st January 2018


Abstract

A recent molecular dynamics simulation study on nanoindentation of diamond carried out by Xu et al. 1 has reported observation of the presence of a controversial hexagonal lonsdaleite phase of carbon in the indentation area. In this comment, we question the reported observation and attribute this anomaly to shortcomings of the long range bond order potential (LCBOP) employed in the nanoindentation study.


In 1967, lonsdaleite (a material named in honour of an Irish crytallographer Ms. Kathleen Lonsdale) was first proposed to be a hexagonal lattice structure allotrope of carbon that rivals cubic diamond in hardness.3 Controversy exists concerning the physical existence of lonsdaleite. Recently, evidence suggesting the physical existence of lonsdaleite was obtained from X-ray diffraction data of pyrolytic graphite subjected to laser shock compression at pressures higher than 170 GPa.4 This evidence arguing that lonsdaleite is a thermodynamic phase by itself has recently been questioned.5 Based on X-ray diffraction patterns,6 it is suggested that lonsdaleite is merely a faulted and twinned (stacking disordered) cubic diamond structure. Theoretical ab initio results7 indicate that the cohesive energy difference per atom between the diamond and lonsdaleite phases is about 51.7 meV.7

Absence of a matured theoretical understanding and sufficient data are why the lonsdaleite phase of carbon is generally not considered in the construction of material constitutive models, particularly interatomic potential functions or force-fields needed for molecular dynamics simulations. An interatomic potential function is usually parameterised and fitted for a given set of phases of the material, but none of the currently available potentials captures the mechanical, structural and energetic aspects of all phases of carbon.8 It is well known that each potential function has its own characteristic advantages and weaknesses, and whether it is applicable or not to a given problem is governed by a range of factors. Only in rare cases and typically by chance a potential may work to describe a phase for which it was not originally fitted. For instance, the analytical bond order potential (ABOP) of Erhart and Albe has been found to best describe the most recently identified phase of penta-graphene9 whilst the EDIP potential was reported most appropriate for simulating amorphous carbons.10

Ideally, MD simulation studies of contact loading processes like nanometric cutting or nanoindentation require a potential to be highly transferable as the material undergoes extreme conditions of stress. For an interatomic potential to correctly reproduce changes in the microstructure or predict phase transitions during contact loading, it is necessary (but generally not sufficient) that the potential function correctly reproduces the cohesive energy of the involved phases of the material, particularly because the incipient plasticity in early stages of wear may occur either due to atom-by-atom attrition, diffusion, or bond breaking.

The above considerations motivated us to examine a series of potentials for carbon proposed in the literature, including the LCBOP function2 employed in the study of Xu et al.,1 to see how closely they describe the cohesive energy difference between cubic and hexagonal phases of carbon. We performed molecular statics calculations at zero pressure to determine the cohesive energies of the diamond and lonsdaleite phases of carbon. Our results shown in Table 1 highlight that it is only the screening incarnation (REBO + S)11 of the reactive empirical bond-order (REBO) potential12,13 predicting energy differences between the diamond and hexagonal phases of carbon that are close to the ab initio energy difference.7 From this, it can be concluded that the occurrence of lonsdaleite observed in the study of Xu et al.1 may be an artefact of the employed LCBOP potential and is likely to have resulted from the underestimation of the structural energy difference. This renders the significance of the reported transformation process questionable.

Table 1 Differences in the cohesive energy per atom between diamond and lonsdaleite phases
Name of potential function Cohesive energy difference between the two phases predicted by the potential (meV per atom) Cohesive energy difference obtained from ab initio calculation (meV per atom)
Tersoff potential14,15 0 51.7 (ref. 7)
ABOP potential16 0
REBO + S function11 41.86
REBO original formulation12,13 −0.04
AIREBO original formulation17 155.9
REAXFF18 6117.9
LCBOP 2 12.48
EDIP carbon19 0


Conclusions

Based on the discussions, we suggest that the appearance of yellowish atoms (referred as lonsdaleite atoms) in the nanoindentation work of Xu et al.1 are mere artefacts.

Conflicts of interest

There are no conflicts to declare.

References

  1. C. Xu, C. Liu and H. Wang, RSC Adv., 2017, 7, 36093–36100 RSC.
  2. J. H. Los and A. Fasolino, Phys. Rev. B: Condens. Matter Mater. Phys., 2003, 68, 024107 CrossRef.
  3. C. Frondel and U. B. Marvin, Nature, 1967, 214, 587–589 CrossRef CAS.
  4. D. Kraus, A. Ravasio, M. Gauthier, D. Gericke, J. Vorberger, S. Frydrych, J. Helfrich, L. Fletcher, G. Schaumann and B. Nagler, Nat. Commun., 2016, 7 DOI:10.1038/ncomms10970.
  5. P. Németh, L. A. J. Garvie, T. Aoki, N. Dubrovinskaia, L. Dubrovinsky and P. R. Buseck, Nat. Commun., 2014, 5 DOI:10.1038/ncomms6447.
  6. C. G. Salzmann, B. J. Murray and J. J. Shephard, Diamond Relat. Mater., 2015, 59, 69–72 CrossRef CAS.
  7. S. Q. Wang and H. Q. Ye, J. Phys.: Condens. Matter, 2003, 15, 5307 CrossRef CAS.
  8. R. Perriot, X. Gu, Y. Lin, V. V. Zhakhovsky and I. I. Oleynik, Phys. Rev. B: Condens. Matter Mater. Phys., 2013, 88, 064101 CrossRef.
  9. S. Winczewski, M. Y. Shaheen and J. Rybicki, Carbon, 2018, 126, 165–175 CrossRef CAS.
  10. C. de Tomas, I. Suarez-Martinez and N. A. Marks, Carbon, 2016, 109, 681–693 CrossRef CAS.
  11. L. Pastewka, A. Klemenz, P. Gumbsch and M. Moseler, Phys. Rev. B: Condens. Matter Mater. Phys., 2013, 87, 205410 CrossRef.
  12. D. W. Brenner, Phys. Rev. B: Condens. Matter Mater. Phys., 1990, 42, 9458–9471 CrossRef CAS.
  13. S. J. Stuart, A. B. Tutein and J. A. Harrison, J. Chem. Phys., 2000, 112, 6472–6486 CrossRef CAS.
  14. J. Tersoff, Phys. Rev. B: Condens. Matter Mater. Phys., 1989, 39, 5566 CrossRef.
  15. J. Tersoff, Phys. Rev. B: Condens. Matter Mater. Phys., 1990, 41, 3248 CrossRef.
  16. P. Erhart and K. Albe, Phys. Rev. B: Condens. Matter Mater. Phys., 2005, 71, 035211 CrossRef.
  17. S. J. Stuart, A. B. Tutein and J. A. Harrison, J. Chem. Phys., 2000, 112, 6472–6486 CrossRef CAS.
  18. A. C. Van Duin, S. Dasgupta, F. Lorant and W. A. Goddard, J. Phys. Chem. A, 2001, 105, 9396–9409 CrossRef CAS.
  19. N. A. Marks, Phys. Rev. B: Condens. Matter Mater. Phys., 2000, 63, 035401 CrossRef.

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