Skip to main content Accessibility help
×
Hostname: page-component-848d4c4894-8kt4b Total loading time: 0 Render date: 2024-06-22T05:15:28.946Z Has data issue: false hasContentIssue false

Chapter 5.2 - Theoretical Search for New Materials – Low-Temperature Compression of Graphitic Layered Materials

Published online by Cambridge University Press:  05 November 2011

S. Tsuneyuki
Affiliation:
University of Tokyo
Y. Tateyama
Affiliation:
National Research Institute for Metals
T. Ogitsu
Affiliation:
University of Tokyo
K. Kusakabe
Affiliation:
Niigata University
Hideo Aoki
Affiliation:
University of Tokyo
Yasuhiko Syono
Affiliation:
Tohoku University, Japan
Get access

Summary

The synthesis of new materials by compressing graphitic layered materials at low temperatures is proposed on the basis of first-principles molecular-dynamics simulations. It is predicted that a class of BCN heterodiamonds are derived from graphite/h-BN superlattices. It is also suggested that compression of a graphite intercalation compound results in an exotic diamond-like material. Differences in layer stacking, intercalants, and stage structures of intercalants in the starting layered materials will result in fruitful variations of the resultant materials.

Introduction

Predicting the structures and properties of materials from a knowledge of their chemical composition has been a long-standing problem of materials science [1]. Thanks to the recent development of computational science approaches, it is often not as difficult to predict stable structure and elctronic properties of even unknown materials theoretically, if we know or assume a rough arrangement of the constituent atoms in the material. It is much more difficult, however, to know how to make it and how stable it is compared with other unknown structures beyond our imagination, as we need overall knowledge of the potential-energy surface in the multidimensional configuration space to do so. An exceptionally simple and hopeful situation for such theoretical designs of materials can be found in the low-temperature compression of crystals.

Some crystals compressed at low (room) temperature undergo structural transformation without atomic diffusion (martensitic transformation), resulting in metastable structures inaccessible at thermal equilibrium or by rapid quenching of high-temperature/pressure phases.

Type
Chapter
Information
Physics Meets Mineralogy
Condensed Matter Physics in the Geosciences
, pp. 299 - 307
Publisher: Cambridge University Press
Print publication year: 2000

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Save book to Kindle

To save this book to your Kindle, first ensure coreplatform@cambridge.org is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

Available formats
×