IntroductionStoichiometric FeS is known to be a natural occurring mineral and has been investigated in fields as diverse as space science [1][2][3], geosciences [4], crystal chemistry [5] and condensed matter physics [6-9], because it is a possible core material for the terrestrial planets and one of the fundamental components of meteorites. Hence, similar to the classical Mott-Hubbard insulator FeO [10,11], FeS is considered to be an important material for solid state and earth sciences. Apart from this, hexagonal iron monosulfide has also been investigated in field as diverse as applied surface sciences [12] or as potential material for future energy storage and lithium-ion battery applications [13].As revealed by high-pressure x-ray diffraction measurements [1,3,5,14], FeS undergoes a series of structural phase transitions with increasing pressure (P): a detailed description of the × P T structural phase transformations of FeS can be found, for example, in [2] and [5]. From these studies it is known that under ambient conditions troilite FeS has a hexagonal structure (space group P − 62c) which is derivative of the NiAs unit cell with axis lengths = =å c 3 5.955 A f and =c 2 11.76 A f [14], where c f is the lattice parameter of the fundamental NiAs subcell. The corresponding crystal structure of troilite FeS is shown in figure 1, see also [14]. As seen in this figure, increasing pressure at room temperature results in a structural phase transition close to 3.5 GPa to an hexagonal NiAs-type structure (here dubbed as h-FeS) [2] with space group P mmc 63 /. With further increasing P at temperatures close to room-T results in an additional structural transformation at around 7 GPa to a monoclinic unit cell (space group P2 1 or P2 1 /m) [14]. It is worth noting as well that the change of the sulfur sublattice might transform the layered structure of tetragonal FeS (mackinawite) to the three-dimensional NiAs-type structure of hexagonal pyrrhotite [15]. Thus, it is clear that FeS adopts a variety of crystallographic structures under different sample preparations [15,16]
AbstractWe present a detailed study of correlation-and pressure-induced electronic reconstruction in hexagonal iron monosulfide, a system which is widely found in meteorites and one of the components of Earth's core. Based on a perusal of experimental data, we stress the importance of multi-orbital electron-electron interactions in concert with first-principles band structure calculations for a consistent understanding of its intrinsic Mott-Hubbard insulating state. We explain the anomalous nature of pressure-induced insulator-metal-insulator transition seen in experiment, showing that it is driven by dynamical spectral weight transfer in response to changes in the crystal-field splittings under pressure. As a byproduct of this analysis, we confirm that the electronic transitions observed in pristine FeS at moderated pressures are triggered by changes in the spin state which causes orbitalselective Kondo quasiparticle electronic reconstruction at lo...