Electron diffraction evidence of domain twinning in graphite-bromine single crystals

D. Ghosh; D. D.L. Chung

doi:10.1016/0025-5408(83)90100-9

Electron diffraction evidence of domain twinning in graphite-bromine single crystals

D. Ghosh
, D. D.L. Chung

Department of Mechanical and Aerospace Engineering

Carnegie Mellon University

Research output: Contribution to journal › Article › peer-review

10 Scopus citations

Abstract

The in-plane electron diffraction pattern from single crystals of graphite-bromine intercalation compound has been interpreted in terms of a three-fold twinned monoclinic unit cell having in-plane lattice translations a=8.87 A ̊, b=4.26 A ̊, and the angle between them γ=103.9°, commensurate with the graphite lattice. The resulting twinned-domain model has been verified by observation of electron diffraction from individual domains.

Original language	English
Pages (from-to)	727-733
Number of pages	7
Journal	Materials Research Bulletin
Volume	18
Issue number	6
DOIs	https://doi.org/10.1016/0025-5408(83)90100-9
State	Published - Jun 1983

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title = "Electron diffraction evidence of domain twinning in graphite-bromine single crystals",

abstract = "The in-plane electron diffraction pattern from single crystals of graphite-bromine intercalation compound has been interpreted in terms of a three-fold twinned monoclinic unit cell having in-plane lattice translations a=8.87 A ̊, b=4.26 A ̊, and the angle between them γ=103.9°, commensurate with the graphite lattice. The resulting twinned-domain model has been verified by observation of electron diffraction from individual domains.",

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year = "1983",

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T1 - Electron diffraction evidence of domain twinning in graphite-bromine single crystals

AU - Ghosh, D.

AU - Chung, D. D.L.

PY - 1983/6

Y1 - 1983/6

N2 - The in-plane electron diffraction pattern from single crystals of graphite-bromine intercalation compound has been interpreted in terms of a three-fold twinned monoclinic unit cell having in-plane lattice translations a=8.87 A ̊, b=4.26 A ̊, and the angle between them γ=103.9°, commensurate with the graphite lattice. The resulting twinned-domain model has been verified by observation of electron diffraction from individual domains.

AB - The in-plane electron diffraction pattern from single crystals of graphite-bromine intercalation compound has been interpreted in terms of a three-fold twinned monoclinic unit cell having in-plane lattice translations a=8.87 A ̊, b=4.26 A ̊, and the angle between them γ=103.9°, commensurate with the graphite lattice. The resulting twinned-domain model has been verified by observation of electron diffraction from individual domains.

UR - https://www.scopus.com/pages/publications/0020763028

U2 - 10.1016/0025-5408(83)90100-9

DO - 10.1016/0025-5408(83)90100-9

M3 - Article

AN - SCOPUS:0020763028

SN - 0025-5408

VL - 18

SP - 727

EP - 733

JO - Materials Research Bulletin

JF - Materials Research Bulletin

IS - 6

ER -

Electron diffraction evidence of domain twinning in graphite-bromine single crystals

Abstract

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