The Fe–Fe 2 P phase diagram at 6 GPa

Daniil A. Minin, Anton F. Shatskiy, Konstantin D. Litasov, Hiroaki Ohfuji

Research output: Contribution to journalArticlepeer-review

10 Citations (Scopus)


Here, we report experimental results on melting and subsolidus phase relations in the Fe–Fe 2 P system at 6 GPa and 900–1600°C. The system has two P-bearing compounds: Fe 3 P and Fe 2 P. X-ray diffraction patterns of these compounds correspond to schreibersite and barringerite, respectively. The Fe–Fe 3 P eutectic appears at 1075°C and 16 mol% P. Schreibersite (Fe 3 P) melts incongruently at 1250°C to produce barringerite (Fe 2 P) and liquid containing 23 mol% P. Barringerite (Fe 2 P) melts congruently at 1575°C. Maximum solid solution of P in metallic iron at 6 GPa is 5 mol%. As temperature increases to 1600°C, the P solubility in the metallic iron decreases to 0.5 mol%, whereas the P content in coexisting liquid decreases to 3 mol%. The composition of quenched phases from Fe–P melt coincides with the compositions of equilibrium phases at corresponding temperature. Consequently, the composition of quenched products of Fe-P melts in meteorites can be used for reconstruction of P–T conditions of their crystallization under ambient or low pressures or during shock melting by impact collisions.

Original languageEnglish
Pages (from-to)50-68
Number of pages19
JournalHigh Pressure Research
Issue number1
Publication statusPublished - 2019 Jan 2


  • barringerite
  • core formation
  • high-pressure
  • Iron
  • meteorites
  • phosphide
  • phosphorus
  • schreibersite


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