Lattice collapse and quenching of magnetism in CaFe2As2 under pressure: A single crystal neutron and x-ray diffraction investigation
arXiv:0811.2013 · doi:10.1103/PhysRevB.79.024513
Abstract
Single crystal neutron and high-energy x-ray diffraction have identified the phase lines corresponding to transitions between the ambient-pressure tetragonal (T), the antiferromagnetic orthorhombic (O) and the non-magnetic collapsed tetragonal (cT) phases of CaFe2As2. We find no evidence of additional structures for pressures up to 2.5 GPa (at 300 K). Both the T-cT and O-cT transitions exhibit significant hysteresis effects and we demonstrate that coexistence of the O and cT phases can occur if a non-hydrostatic component of pressure is present. Measurements of the magnetic diffraction peaks show no change in the magnetic structure or ordered moment as a function of pressure in the O phase and we find no evidence of magnetic ordering in the cT phase. Band structure calculations show that the transition results in a strong decrease of the iron 3d density of states at the Fermi energy, consistent with a loss of the magnetic moment.
List of authors in metadata and typos in labeling of inset in Fig. 1(a) corrected. One ref. added. No other changes
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- Topological change of the Fermi surface in ternary iron-pnictides with reduced c/a ratio: A dHvA study of CaFe2P2
- Microscopic origin of pressure-induced phase transitions in iron-pnictide superconductors: an {ab initio} molecular-dynamics study
- Successive phase transitions under high pressure in FeTe0.92
- NMR investigation of superconductivity and antiferromagnetism in CaFeAs under pressure
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