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| Hauptseite > Publikationsdatenbank > Evaluation of Thermodynamic Data and Phase Equlibria in the System Ca-Cr-Cu-Fe-Mg-Mn-S. Part II: Ternary and Quasi-Ternary Subsystems > print |
| Hauptseite > Publikationsdatenbank > Evaluation of Thermodynamic Data and Phase Equlibria in the System Ca-Cr-Cu-Fe-Mg-Mn-S. Part II: Ternary and Quasi-Ternary Subsystems > print |
| 001 | 829832 | ||
| 005 | 20240711092233.0 | ||
| 024 | 7 | _ | |a 10.1016/j.calphad.2017.01.007 |2 doi |
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| 100 | 1 | _ | |a Jantzen, T. |0 P:(DE-HGF)0 |b 0 |e Corresponding author |
| 245 | _ | _ | |a Evaluation of Thermodynamic Data and Phase Equlibria in the System Ca-Cr-Cu-Fe-Mg-Mn-S. Part II: Ternary and Quasi-Ternary Subsystems |
| 260 | _ | _ | |a Amsterdam [u.a.] |c 2017 |b Elsevier Science |
| 336 | 7 | _ | |a article |2 DRIVER |
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| 520 | _ | _ | |a The Ca-Cr-Cu-Fe-Mg-Mn-S system has been thermodynamically assessed using all available experimental data. Sulfur is introduced into the thermodynamic description of 8 solid solution phases such as Thiospinel, Digenite, Oldhamite, Cu2S-I, Cu2S-II, Pyrrhotite, Brezinaite, Chalcopyrite-HT using available experimental information. Particular attention was given to the phase Pyrrhotite which forms at high temperatures a solid solution with end-members Fe1−xS and Cr1−xS in the ternary Cr-Fe-S system, and also the phase Digenite, which exhibits very wide solubility toward Pyrrhotite in the Cu-Fe-S system. In this part of the report ternary and quasi-ternary subsystems are presented while all relevant binary systems as well as pseudo-binary sections have already been presented in Part I of this series. |
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