Numerical simulation of surface and bulk deformation in three-dimensional polycrystals

V. A. Romanova, Ruslan Revovich Balokhonov

Research output: Contribution to journalArticle

7 Citations (Scopus)

Abstract

The paper presents the results of numerical analysis of mesoscale deformation in three-dimensional polycrystals under tension. The three-dimensional models of polycrystalline structures are generated by a step-by-step packing method. Elastoplastic grain response is described taking into account the Hall-Petch relation, strain hardening and elastic anisotropy at the mesolevel. The nucleation and development of plastic shear strains on the surface and in the bulk of polycrystalline specimens are studied in a numerical experiment. The role of free surface and grain boundaries in the evolution of mesoscale deformation is analyzed.

Original languageEnglish
Pages (from-to)130-140
Number of pages11
JournalPhysical Mesomechanics
Volume12
Issue number3-4
DOIs
Publication statusPublished - 2009
Externally publishedYes

Fingerprint

Polycrystals
polycrystals
elastic anisotropy
strain hardening
shear strain
Shear strain
Computer simulation
three dimensional models
Strain hardening
numerical analysis
Numerical analysis
Grain boundaries
Anisotropy
Nucleation
plastics
grain boundaries
simulation
nucleation
Plastics
anisotropy

Keywords

  • 3D model
  • numerical simulation
  • plastic deformation
  • polycrystalline structure

ASJC Scopus subject areas

  • Condensed Matter Physics
  • Surfaces and Interfaces
  • Mechanics of Materials
  • Materials Science(all)

Cite this

Numerical simulation of surface and bulk deformation in three-dimensional polycrystals. / Romanova, V. A.; Balokhonov, Ruslan Revovich.

In: Physical Mesomechanics, Vol. 12, No. 3-4, 2009, p. 130-140.

Research output: Contribution to journalArticle

Romanova, V. A. ; Balokhonov, Ruslan Revovich. / Numerical simulation of surface and bulk deformation in three-dimensional polycrystals. In: Physical Mesomechanics. 2009 ; Vol. 12, No. 3-4. pp. 130-140.
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