Shock-formed carbon materials with intergrown sp 3 - and sp 2 -bonded nanostructured units

Author:

Németh Péter1ORCID,Lancaster Hector J.2ORCID,Salzmann Christoph G.3ORCID,McColl Kit4,Fogarassy Zsolt5,Garvie Laurence A. J.6,Illés Levente5,Pécz Béla5ORCID,Murri Mara7ORCID,Corà Furio3,Smith Rachael L.3,Mezouar Mohamed8ORCID,Howard Christopher A.2ORCID,McMillan Paul F.3ORCID

Affiliation:

1. Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences (MTA Centre of Excellence), Eötvös Loránd Research Network, H-1112 Budapest, Hungary

2. Department of Physics & Astronomy, University College London, London WC1E 6BT, United Kingdom

3. Department of Chemistry, University College London, London WC1H 0AJ, United Kingdom

4. Department of Chemistry, University of Bath, Bath BA2 7AX, United Kingdom

5. Institute of Technical Physics and Materials Science, Centre for Energy Research (MTA Centre of Excellence), Eötvös Loránd Research Network, H-1121 Budapest, Hungary

6. Buseck Center for Meteorite Studies, Arizona State University, Tempe, AZ 85287

7. Department of Earth and Environmental Sciences, University of Milano-Bicocca, 20126 Milano, Italy

8. Experiments Division, European Synchrotron Radiation Facility, Grenoble 38000, France

Abstract

Studies of dense carbon materials formed by bolide impacts or produced by laboratory compression provide key information on the high-pressure behavior of carbon and for identifying and designing unique structures for technological applications. However, a major obstacle to studying and designing these materials is an incomplete understanding of their fundamental structures. Here, we report the remarkable structural diversity of cubic/hexagonally ( c / h ) stacked diamond and their association with diamond-graphite nanocomposites containing sp 3 -/sp 2 -bonding patterns, i.e., diaphites, from hard carbon materials formed by shock impact of graphite in the Canyon Diablo iron meteorite. We show evidence for a range of intergrowth types and nanostructures containing unusually short (0.31 nm) graphene spacings and demonstrate that previously neglected or misinterpreted Raman bands can be associated with diaphite structures. Our study provides a structural understanding of the material known as lonsdaleite, previously described as hexagonal diamond, and extends this understanding to other natural and synthetic ultrahard carbon phases. The unique three-dimensional carbon architectures encountered in shock-formed samples can place constraints on the pressure–temperature conditions experienced during an impact and provide exceptional opportunities to engineer the properties of carbon nanocomposite materials and phase assemblages.

Publisher

Proceedings of the National Academy of Sciences

Subject

Multidisciplinary

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