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@ARTICLE{Pavlychkov:173005,
      author       = {Pavlychkov, D. and Przepiorzynski, B. and Kowalski, W. and
                      Velikanova, T. and Grushko, Benjamin},
      title        = {{A}l-{C}r-{F}e phase diagram. {I}sothermal sections in the
                      region above 50 $at\%$ {A}l.},
      journal      = {Calphad},
      volume       = {45},
      issn         = {0364-5916},
      address      = {Amsterdam [u.a.]},
      publisher    = {Elsevier Science},
      reportid     = {FZJ-2014-06419},
      pages        = {194 - 203},
      year         = {2014},
      abstract     = {The Al–Cr–Fe phase diagram was studied in the
                      compositional range of 50–100 $at\%$ Al and partial
                      isothermal sections were determined at 1160, 1100, 1075,
                      1042, 1000, 900, 800 and 700 °C. In the low-Al part of the
                      studied compositional region the isostructural
                      high-temperature Al–Cr and Al–Fe γ1-phases form a
                      continuous region of solid solutions. Both binary Al13Fe4
                      and Al5Fe2 were found to dissolve up to 6.5 $at\%$ Cr while
                      Al2Fe was found to extend up to 4.1 $at\%$ Cr. The solid
                      solutions based on the Al–Cr γ2 and μ phases were
                      determined to reach 35.2 and 1.3 $at\%$ Fe, respectively.
                      The dissolution of Cr in the Al–Fe binaries only slightly
                      influences their Al concentrations, while the Al–Cr
                      binaries exhibit decreasing Al concentration with increasing
                      Fe concentration. The Al–Cr η-phase dissolves up to 5
                      $at\%$ Fe, which results in a sharp decrease of its Al
                      concentration and increase of melting temperatures. The
                      earlier reported existence of a ternary decagonal D3-phase
                      and three complex periodic phases O1, H and ε was confirmed
                      and their compositions at different temperatures were
                      specified.},
      cin          = {PGI-5},
      ddc          = {540},
      cid          = {I:(DE-Juel1)PGI-5-20110106},
      pnm          = {424 - Exploratory materials and phenomena (POF2-424)},
      pid          = {G:(DE-HGF)POF2-424},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000337880600017},
      doi          = {10.1016/j.calphad.2013.12.007},
      url          = {https://juser.fz-juelich.de/record/173005},
}