Pressure-induced phase transitions of AX2-type iron pnictides: an ab initio study

An investigation into the high-pressure behavior of AX2-type iron pnictides was conducted using first-principles calculations based on density functional theory within the generalized gradient approximation. Our results demonstrate that a phase transition from the marcasite to the CuAl2 occurs at 108 GPa for FeP2, at 92 GPa for FeAs2, and at 38 GPa for FeSb2, accompanying a semiconductor-to-metal crossover. A linear relationship between bulk moduli and the inverse specific volume is proposed to be B0 = 17 498/V0−45.9 GPa for the marcasite-type phase and B0 = 31 798/V0−67.5 GPa for the CuAl2-type phase. According to the observed structural evolutions, we claim that the regular marcasite transforms to the CuAl2-type phase and the anomalous marcasite transforms to the pyrite-type phase at high pressures.

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