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Materials Data on Fe2S by Materials Project

FeFeS crystallizes in the triclinic P1 space group. The structure is three-dimensional. there are fourteen inequivalent Fe sites. In the first Fe site, Fe is bonded in a distorted bent 150 degrees geometry to two S atoms. There are one shorter (2.23 Å) and one longer (2.28 Å) Fe–S bond lengths. In the second Fe site, Fe is bonded in a 2-coordinate geometry to three S atoms. There are a spread of Fe–S bond distances ranging from 2.30–2.64 Å. In the third Fe site, Fe is bonded in a 2-coordinate geometry to four S atoms. There are a spread of Fe–S bond distances ranging from 2.26–2.62 Å. In the fourth Fe site, Fe is bonded in a 3-coordinate geometry to three S atoms. There are a spread of Fe–S bond distances ranging from 2.30–2.32 Å. In the fifth Fe site, Fe is bonded in a 3-coordinate geometry to three S atoms. There are a spread of Fe–S bond distances ranging from 2.15–2.21 Å. In the sixth Fe site, Fe is bonded in a 3-coordinate geometry to three S atoms. There are one shorter (2.23 Å) and two longer (2.29 Å) Fe–S bond lengths. In the seventh Fe site, Fe is bonded in a 3-coordinate geometry to three S atoms. There are one shorter (2.28 Å) and two longer (2.37 Å) Fe–S bond lengths. In the eighth Fe site, Fe is bonded in a 3-coordinate geometry to three S atoms. All Fe–S bond lengths are 2.25 Å. In the ninth Fe site, Fe is bonded in a 3-coordinate geometry to three S atoms. There are two shorter (2.24 Å) and one longer (2.34 Å) Fe–S bond lengths. In the tenth Fe site, Fe is bonded in a 4-coordinate geometry to four S atoms. There are a spread of Fe–S bond distances ranging from 2.25–2.56 Å. In the eleventh Fe site, Fe is bonded in a 3-coordinate geometry to three S atoms. There are a spread of Fe–S bond distances ranging from 2.32–2.48 Å. In the twelfth Fe site, Fe is bonded in a distorted trigonal non-coplanar geometry to three S atoms. There are a spread of Fe–S bond distances ranging from 2.16–2.20 Å. In the thirteenth Fe site, Fe is bonded in a distorted rectangular see-saw-like geometry to four S atoms. There are a spread of Fe–S bond distances ranging from 2.20–2.22 Å. In the fourteenth Fe site, Fe is bonded in a 1-coordinate geometry to three equivalent S atoms. There are a spread of Fe–S bond distances ranging from 2.34–2.60 Å. There are seven inequivalent S sites. In the first S site, S is bonded in a 5-coordinate geometry to five Fe atoms. In the second S site, S is bonded in a 5-coordinate geometry to five Fe atoms. In the third S site, S is bonded in a 7-coordinate geometry to seven Fe atoms. In the fourth S site, S is bonded in a 6-coordinate geometry to six Fe atoms. In the fifth S site, S is bonded in a 7-coordinate geometry to seven Fe atoms. In the sixth S site, S is bonded in a 6-coordinate geometry to six Fe atoms. In the seventh S site, S is bonded in a 5-coordinate geometry to eight Fe atoms.

36 MATERIALS SCIENCE↗

Materials Data on Fe2S by Materials Project

FeFeS crystallizes in the monoclinic Cm space group. The structure is three-dimensional. there are fourteen inequivalent Fe sites. In the first Fe site, Fe is bonded in a distorted bent 150 degrees geometry to two S atoms. There are one shorter (2.14 Å) and one longer (2.18 Å) Fe–S bond lengths. In the second Fe site, Fe is bonded in a 4-coordinate geometry to four S atoms. There are a spread of Fe–S bond distances ranging from 2.21–2.42 Å. In the third Fe site, Fe is bonded in a 3-coordinate geometry to three S atoms. There are one shorter (2.24 Å) and two longer (2.32 Å) Fe–S bond lengths. In the fourth Fe site, Fe is bonded in a 1-coordinate geometry to three S atoms. There are one shorter (2.22 Å) and two longer (2.56 Å) Fe–S bond lengths. In the fifth Fe site, Fe is bonded in a 3-coordinate geometry to three S atoms. There are one shorter (2.18 Å) and two longer (2.19 Å) Fe–S bond lengths. In the sixth Fe site, Fe is bonded in a 3-coordinate geometry to three S atoms. There are one shorter (2.18 Å) and two longer (2.23 Å) Fe–S bond lengths. In the seventh Fe site, Fe is bonded in a 3-coordinate geometry to three S atoms. There are two shorter (2.19 Å) and one longer (2.20 Å) Fe–S bond lengths. In the eighth Fe site, Fe is bonded in a 3-coordinate geometry to three S atoms. There are two shorter (2.21 Å) and one longer (2.22 Å) Fe–S bond lengths. In the ninth Fe site, Fe is bonded in a 3-coordinate geometry to three S atoms. There are one shorter (2.26 Å) and two longer (2.27 Å) Fe–S bond lengths. In the tenth Fe site, Fe is bonded in a 3-coordinate geometry to three S atoms. All Fe–S bond lengths are 2.25 Å. In the eleventh Fe site, Fe is bonded in a 3-coordinate geometry to three S atoms. There are two shorter (2.21 Å) and one longer (2.26 Å) Fe–S bond lengths. In the twelfth Fe site, Fe is bonded in a 3-coordinate geometry to three S atoms. There are two shorter (2.28 Å) and one longer (2.31 Å) Fe–S bond lengths. In the thirteenth Fe site, Fe is bonded in a rectangular see-saw-like geometry to four S atoms. There are two shorter (2.21 Å) and two longer (2.35 Å) Fe–S bond lengths. In the fourteenth Fe site, Fe is bonded in a distorted trigonal non-coplanar geometry to three S atoms. There are two shorter (2.18 Å) and one longer (2.20 Å) Fe–S bond lengths. There are seven inequivalent S sites. In the first S site, S is bonded to six Fe atoms to form distorted edge-sharing SFe6 pentagonal pyramids. In the second S site, S is bonded in a 6-coordinate geometry to six Fe atoms. In the third S site, S is bonded to six Fe atoms to form distorted edge-sharing SFe6 pentagonal pyramids. In the fourth S site, S is bonded to six Fe atoms to form distorted edge-sharing SFe6 pentagonal pyramids. In the fifth S site, S is bonded to six Fe atoms to form distorted edge-sharing SFe6 pentagonal pyramids. In the sixth S site, S is bonded to six Fe atoms to form distorted edge-sharing SFe6 pentagonal pyramids. In the seventh S site, S is bonded in a 7-coordinate geometry to seven Fe atoms.

36 MATERIALS SCIENCE↗

The crystal structure of Fe2S at 90 GPa based on single-crystal X-ray diffraction techniques

The Fe-S system was explored in a laser-heated diamond-anvil cell at 89(2) GPa and 2380(120) K to better understand the phase stability of Fe 2 S. Upon temperature quenching, crystallites of Fe 2 S were identified, and their structure was investigated using single-crystal X-ray diffraction techniques. At these conditions, Fe 2 S adopts the C23 structure (anti-PbCl 2 , Co 2 P) with space group Pnma (Z = 4). This structure consists of columns of corner-sharing, FeS 4 tetrahedra, and columns of edge-sharing FeS 5 square pyramids linked along edges in the b direction. Sulfur is in ninefold coordination with Fe. This work marks the first high-pressure structural solution and refinement of Fe 2 S synthesized in a multigrain Fe+FeS sample at 90 GPa and 2400 K and establishes the stability of C23 Fe 2 S at these conditions. A previous powder diffraction study reports an orthorhombic Fe 2 S phase with a C37, Co 2 Si-like unit cell above 190 GPa. A C23–C37 structural transition is inferred to explain the previously observed unit-cell parameters at higher pressures and temperatures. These results highlight the utility of applying single-crystal X-ray diffraction techniques to high P-T multigrain samples to explore the structural properties of iron-rich phases in Earth and planetary cores.

36 MATERIALS SCIENCE↗