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@ARTICLE{daSilva:622846,
      author       = {da Silva, Carlos Samuel Alves and Rabelo Coutinho Saraiva,
                      Breno and Novotný, Ladislav and Sarvezuk, Paulo Willian
                      Carvalho and Masoumi, Mohammad and Silva, Cleiton Carvalho
                      and Herculano, Luis Flávio Gaspar and Cardoso, Jorge Luiz
                      and de Abreu, Hamilton Ferreira Gomes and Beres, Miloslav},
      title        = {{T}exture and lattice strain evolution in a pearlitic steel
                      during shear deformation: {A}n in situ synchrotron {X}-ray
                      diffraction study},
      journal      = {International journal of plasticity},
      volume       = {181},
      issn         = {0749-6419},
      address      = {Frankfurt, M. [u.a.]},
      publisher    = {Pergamon Press},
      reportid     = {PUBDB-2025-00526},
      pages        = {104083},
      year         = {2024},
      note         = {Waiting for fulltext},
      abstract     = {In-situ synchrotron X-ray diffraction experiments were
                      conducted on the pearlitic steel sample with a carbon
                      content of $0.74\%$ by weight. Specimens were subjected to
                      uniaxial loading that induced shear deformation and
                      two-dimensional diffraction patterns were acquired. The
                      evolution of the lattice microstrain and the strain-resolved
                      crystallographic texture development of both ferrite
                      (α-BCC) and cementite (θ-orthorhombic) phases were
                      followed. The analysis revealed that the texture changed
                      from {110}<113>α to {113}<121>α component and then,
                      stabilized at {013}<uvw>α orientations. The θ phase
                      exhibited a weak texture in the {100, 010, and 001}θ family
                      planes. Additionally, it was revealed that the nucleation of
                      interfacial defects at the α/θ interface promotes the
                      amorphization of cementite and the activation of slip
                      systems in less densely packed {310}α planes. The influence
                      of microstructural changes on mechanical properties is
                      discussed.},
      cin          = {DOOR ; HAS-User / Hereon / FS-NL},
      ddc          = {530},
      cid          = {I:(DE-H253)HAS-User-20120731 / I:(DE-H253)Hereon-20210428 /
                      I:(DE-H253)FS-NL-20120731},
      pnm          = {6G3 - PETRA III (DESY) (POF4-6G3) / FS-Proposal: I-20211274
                      (I-20211274)},
      pid          = {G:(DE-HGF)POF4-6G3 / G:(DE-H253)I-20211274},
      experiment   = {EXP:(DE-H253)P-P07-20150101 /
                      EXP:(DE-H253)Nanolab-04-20150101},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:001302757800001},
      doi          = {10.1016/j.ijplas.2024.104083},
      url          = {https://bib-pubdb1.desy.de/record/622846},
}