Subgrain Rotation Recrystallization During Shearing

Insights From Full-Field Numerical Simulations of Halite Polycrystals

E Gomez Rivas, A Griera, M-G Llorens, P D Bons, R A Lebensohn, S Piazolo

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Abstract

We present, for the first time, results of full-field numerical simulations of subgrain rotation recrystallization of halite polycrystals during simple shear deformation. The series of simulations show how microstructures are controlled by the competition between (i) grain size reduction by creep by dislocation glide and (ii) intracrystalline recovery encompassing subgrain coarsening (SGC) by coalescence through rotation and alignment of the lattices of neighboring subgrains. A strong grain size reduction develops in models without intracrystalline recovery, as a result of the formation of high-angle grain boundaries when local misorientations exceed 15°. The activation of subgrain coarsening associated with recovery decreases the stored strain energy and results in grains with low intracrystalline heterogeneities. However, this type of recrystallization does not significantly modify crystal preferred orientations. Lattice orientation and grain boundary maps reveal that this full-field modelling approach is able to successfully reproduce the evolution of dry halite microstructures from laboratory deformation experiments, thus opening new opportunities in this field of research. We demonstrate how the mean subgrain boundary misorientations can be used to estimate the strain accommodated by dislocation glide using a universal scaling exponent of about 2/3, as predicted by theoretical models. In addition, this strain gauge can be potentially applied to estimate the intensity of intracrystalline recovery, associated with temperature, using quantitative crystallographic analyses in areas with strain gradients.
Original languageEnglish
Pages (from-to)8810-8827
Number of pages18
JournalJournal of Geophysical Research
Volume122
Issue number11
Early online date3 Nov 2017
DOIs
Publication statusPublished - Nov 2017

Fingerprint

Polycrystals
halite
polycrystals
Sodium chloride
shearing
Shearing
recovery
Recovery
Computer simulation
Coarsening
grain boundary
dislocation
misalignment
Crystal orientation
simulation
microstructure
Grain boundaries
grain size
grain boundaries
Microstructure

Keywords

  • subgrain rotation recrystallization
  • intracrystalline recovery
  • halite
  • misorientation
  • shearing
  • strain gauge

Cite this

Subgrain Rotation Recrystallization During Shearing : Insights From Full-Field Numerical Simulations of Halite Polycrystals. / Gomez Rivas, E; Griera, A; Llorens, M-G; Bons, P D; Lebensohn, R A; Piazolo, S.

In: Journal of Geophysical Research, Vol. 122, No. 11, 11.2017, p. 8810-8827.

Research output: Contribution to journalArticle

Gomez Rivas, E ; Griera, A ; Llorens, M-G ; Bons, P D ; Lebensohn, R A ; Piazolo, S. / Subgrain Rotation Recrystallization During Shearing : Insights From Full-Field Numerical Simulations of Halite Polycrystals. In: Journal of Geophysical Research. 2017 ; Vol. 122, No. 11. pp. 8810-8827.
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AB - We present, for the first time, results of full-field numerical simulations of subgrain rotation recrystallization of halite polycrystals during simple shear deformation. The series of simulations show how microstructures are controlled by the competition between (i) grain size reduction by creep by dislocation glide and (ii) intracrystalline recovery encompassing subgrain coarsening (SGC) by coalescence through rotation and alignment of the lattices of neighboring subgrains. A strong grain size reduction develops in models without intracrystalline recovery, as a result of the formation of high-angle grain boundaries when local misorientations exceed 15°. The activation of subgrain coarsening associated with recovery decreases the stored strain energy and results in grains with low intracrystalline heterogeneities. However, this type of recrystallization does not significantly modify crystal preferred orientations. Lattice orientation and grain boundary maps reveal that this full-field modelling approach is able to successfully reproduce the evolution of dry halite microstructures from laboratory deformation experiments, thus opening new opportunities in this field of research. We demonstrate how the mean subgrain boundary misorientations can be used to estimate the strain accommodated by dislocation glide using a universal scaling exponent of about 2/3, as predicted by theoretical models. In addition, this strain gauge can be potentially applied to estimate the intensity of intracrystalline recovery, associated with temperature, using quantitative crystallographic analyses in areas with strain gradients.

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