Ce–Cr system

13 accepted literature values from 1 paper(s) (experimental 6, model 4, unspecified 3); 1 calculated phase diagram(s). 4 further extracted value(s) not accepted by the reader-agreement checks are only in the JSON/CSV.

Data: JSON · CSV · interactive explorer · interactive phase diagram · phases (5) · papers (bibliography) · Markdown

Accepted values by evidence class
Evidence classValues
experimental6
model4
unspecified3
Accepted values by property group
Property groupValues
invariant reaction13

Calculated phase diagrams

Binary phase diagrams calculated with pycalphad 0.11.2 from the SGTE binary collection (Hallstedt 2025, CC BY 4.0). Evidence class: model.

Assessments with a calculated phase diagram
TDB fileAssessmentSHA-256Links
CeCr-09Cha.tdbW. Chan, C. Gao, O.N. Dogan, P. King, A.D. Rollett, J. Phase Equilib. Diffus., 30, 578-86(2009). doi:10.1007/s11669-009-9581-397d439b83a4d8aa04871403257901aba4dc8d47e5f49459cf2c8289ab2fdb239viewer · TDB · JSON
Calculated three-phase invariants (model, mole fraction of the second component)
TDB fileT (K)Phases at the invariant
CeCr-09Cha.tdb2052.62LIQUID (x(Cr) 0.33349) + LIQUID#2 (x(Cr) 0.86514) + BCC_A2 (x(Cr) 0.97707)
CeCr-09Cha.tdb1054.24BCC_A2#2 (x(Cr) 0.0182) + LIQUID (x(Cr) 0.02403) + BCC_A2 (x(Cr) 0.99904)
CeCr-09Cha.tdb988.98FCC_A1 (x(Cr) 0.00659) + BCC_A2#2 (x(Cr) 0.01229) + BCC_A2 (x(Cr) 0.9994)

Convex hulls: Materials Project DFT hull · OQMD DFT hull

Invariant reactions (literature)

Invariant reactions reported in the literature for the Ce–Cr system (13)
T (K)Reaction / phasesCompositions (mole fraction)ClassSourceLocationQuote
2092.55monotectic: L1 -> L2 + CrL1: Ce 0.039; L2: Ce 0.961unspecified[1] Chan 2009
cites Ray 2009
Table 2, p. 5, row 3
report
2063.15monotectic: L1 -> L2 + CrL1: Ce 0.0185; L2: Ce 0.71; Cr: Ce 0.0125experimental[1] Chan 2009
cites Massalski 1990
Table 2, p. 5, row 2
report
2053.15monotectic: L1 -> L2 + CrL1: Ce 0.0482; Cr: Ce 0.0272experimental[1] Chan 2009
cites Savitskii 1959
Table 2, p. 5, row 1
report
2052.15monotectic: L1 -> L2 + CrL1: Ce 0.135; L2: Ce 0.667; Cr: Ce 0.023model[1] Chan 2009Table 2, p. 5, row 4
report
1070.65eutectic: L2 -> Cr + δCeL2: Ce 0.9998unspecified[1] Chan 2009
cites Ray 2009
Table 2, p. 5, row 8
report
1058.15eutectic: L2 -> Cr + δCeL2: Ce 0.95; Cr: Ce 0; δCe: Ce 0.985experimental[1] Chan 2009
cites Massalski 1990
Table 2, p. 5, row 6
report
1054.15eutectic: L2 -> Cr + δCeL2: Ce 0.976; Cr: Ce 0.001; δCe: Ce 0.982model[1] Chan 2009Table 2, p. 5, row 9
report
1053.15eutectic: L2 -> Cr + δCeexperimental[1] Chan 2009
cites Savitskii 1959
Table 2, p. 5, row 5
report
1044.15eutectic: L2 -> Cr + δCeL2: Ce 0.9826unspecified[1] Chan 2009
cites Terekhova 1990
Table 2, p. 5, row 7
report
989.15δCe -> Cr + γCeδCe: Ce 0.988; Cr: Ce 6.000e-4; γCe: Ce 0.993model[1] Chan 2009Table 2, p. 5, row 11
report
988.15δCe -> Cr + γCeδCe: Ce 0.99; Cr: Ce 0; γCe: Ce 0.995experimental[1] Chan 2009
cites Massalski 1990
Table 2, p. 5, row 10
report
334.15γCe -> Cr + αCeγCe: Ce 1; Cr: Ce 0model[1] Chan 2009Table 2, p. 5, row 13
report
334.15γCe -> Cr + αCeexperimental[1] Chan 2009
cites Massalski 1990
Table 2, p. 5, row 12
report

Sources

Reporting papers the values were read from (a value cited from another work names that work in its row).

  1. Wren Chan, Michael C. Gao, Ömer N. Doğan, Paul King, Anthony D. Rollett, Thermodynamic Assessment of Cr-Rare Earth Systems, J. Phase Equilib. Diffus. 30, 578-586 (2009). doi:10.1007/s11669-009-9581-3