Abstract
All studied properties of FeX (X = Pt, Pd) in austenitic and martensitic phases are investigated within Local Spin Density Approximation as exchange functional. The structural parameters at equilibrium for ferromagnetic tetragonal FePt and FePd a = 3.911 Å, c = 3.842 Å and a = 3.816 Å, c = 3.736 Å, and the lattice constant for ferromagnetic cubic FePt and FePd a = 4.9304 Å and a = 4.905 Å agree well with their available theoretical and experimental data. FePd and FePt formation enthalpy of the martensitic phase was −12625.73 eV and −39414.97 eV, while in the austenitic phase it was −12625.33 eV and −39413.97 eV. The rock-salt FePd (tetragonal FePt) is more stable than tetragonal FePd (rock-salt FePt). For both compounds, the anisotropy is more pronounced in the martensitic phase.
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