Search NASA⌕ Search

DOE OSTI · 1750506

Materials Data on Fe7SiO10 by Materials Project

Abstract

Fe7SiO10 crystallizes in the monoclinic Cm space group. The structure is three-dimensional. there are seven inequivalent Fe+2.29+ sites. In the first Fe+2.29+ site, Fe+2.29+ is bonded to six O2- atoms to form FeO6 octahedra that share a cornercorner with one FeO6 octahedra, corners with two equivalent FeO4 tetrahedra, corners with four equivalent SiO4 tetrahedra, and edges with six FeO6 octahedra. The corner-sharing octahedral tilt angles are 1°. There are a spread of Fe–O bond distances ranging from 2.02–2.27 Å. In the second Fe+2.29+ site, Fe+2.29+ is bonded to six O2- atoms to form FeO6 octahedra that share a cornercorner with one FeO6 octahedra, corners with two equivalent SiO4 tetrahedra, corners with four equivalent FeO4 tetrahedra, and edges with six FeO6 octahedra. The corner-sharing octahedral tilt angles are 4°. There are a spread of Fe–O bond distances ranging from 2.11–2.35 Å. In the third Fe+2.29+ site, Fe+2.29+ is bonded to six O2- atoms to form FeO6 octahedra that share corners with four equivalent FeO6 octahedra, a cornercorner with one FeO4 tetrahedra, and edges with ten FeO6 octahedra. The corner-sharing octahedra tilt angles range from 3–10°. There are a spread of Fe–O bond distances ranging from 2.00–2.11 Å. In the fourth Fe+2.29+ site, Fe+2.29+ is bonded to six O2- atoms to form FeO6 octahedra that share corners with four equivalent FeO6 octahedra, a cornercorner with one SiO4 tetrahedra, and edges with ten FeO6 octahedra. The corner-sharing octahedra tilt angles range from 3–16°. There are a spread of Fe–O bond distances ranging from 2.08–2.22 Å. In the fifth Fe+2.29+ site, Fe+2.29+ is bonded to six O2- atoms to form FeO6 octahedra that share corners with five FeO6 octahedra, a cornercorner with one FeO4 tetrahedra, and edges with ten FeO6 octahedra. The corner-sharing octahedra tilt angles range from 1–10°. There are a spread of Fe–O bond distances ranging from 2.07–2.35 Å. In the sixth Fe+2.29+ site, Fe+2.29+ is bonded to six O2- atoms to form FeO6 octahedra that share corners with five FeO6 octahedra, a cornercorner with one SiO4 tetrahedra, and edges with ten FeO6 octahedra. The corner-sharing octahedra tilt angles range from 3–16°. There are a spread of Fe–O bond distances ranging from 2.10–2.28 Å. In the seventh Fe+2.29+ site, Fe+2.29+ is bonded to four O2- atoms to form FeO4 tetrahedra that share corners with eight FeO6 octahedra and corners with two equivalent FeO4 tetrahedra. The corner-sharing octahedra tilt angles range from 54–61°. There are a spread of Fe–O bond distances ranging from 1.89–1.91 Å. Si4+ is bonded to four O2- atoms to form SiO4 tetrahedra that share corners with eight FeO6 octahedra and corners with two equivalent SiO4 tetrahedra. The corner-sharing octahedra tilt angles range from 53–60°. There are a spread of Si–O bond distances ranging from 1.63–1.75 Å. There are ten inequivalent O2- sites. In the first O2- site, O2- is bonded in a trigonal planar geometry to one Fe+2.29+ and two equivalent Si4+ atoms. In the second O2- site, O2- is bonded in a trigonal planar geometry to three Fe+2.29+ atoms. In the third O2- site, O2- is bonded to five Fe+2.29+ atoms to form OFe5 square pyramids that share corners with four equivalent OFe6 octahedra, a cornercorner with one OFe4 trigonal pyramid, edges with four OFe6 octahedra, and edges with four OFe5 square pyramids. The corner-sharing octahedra tilt angles range from 6–8°. In the fourth O2- site, O2- is bonded to five Fe+2.29+ atoms to form OFe5 square pyramids that share corners with four equivalent OFe6 octahedra, corners with four OFe4 trigonal pyramids, edges with four OFe6 octahedra, and edges with four OFe5 square pyramids. The corner-sharing octahedral tilt angles are 5°. In the fifth O2- site, O2- is bonded to six Fe+2.29+ atoms to form OFe6 octahedra that share corners with four equivalent OFe5 square pyramids, a cornercorner with one OFe4 trigonal pyramid, edges with four OFe6 octahedra, and edges with four OFe5 square pyramids. In the sixth O2- site, O2- is bonded to six Fe+2.29+ atoms to form OFe6 octahedra that share corners with four equivalent OFe5 square pyramids, edges with four OFe6 octahedra, edges with four OFe5 square pyramids, and edges with four OFe4 trigonal pyramids. In the seventh O2- site, O2- is bonded to four Fe+2.29+ atoms to form distorted OFe4 trigonal pyramids that share corners with three OFe5 square pyramids, corners with five OFe4 trigonal pyramids, edges with two equivalent OFe6 octahedra, and an edgeedge with one OFe4 trigonal pyramid. In the eighth O2- site, O2- is bonded in a distorted rectangular see-saw-like geometry to three Fe+2.29+ and one Si4+ atom. In the ninth O2- site, O2- is bonded to four Fe+2.29+ atoms to form distorted OFe4 trigonal pyramids that share a cornercorner with one OFe6 octahedra, corners with two equivalent OFe5 square pyramids, corners with five OFe4 trigonal pyramids, edges with two equivalent OFe6 octahedra, and an edgeedge with one OFe4 trigonal pyramid. The corner-sharing octahedral tilt angles are 4°. In the tenth O2- site, O2- is bonded in a rectangular see-saw-like geometry to three Fe+2.29+ and one Si4+ atom.

Explore related subjects

Keep this discovery

Explore connections, maps & timelines

BibTeXRIS

2020-05-02. Materials Data on Fe7SiO10 by Materials Project. https://doi.org/10.17188/1750506

Cite the original work for its findings. Save a collection to share your selection of sources.

KEEP EXPLORING

Related reports

Cyclic moisture reactivation of calcium sorbents for long duration thermochemical energy storage

The transition to a flexible and reliable energy infrastructure, using electro-thermal energy generation technologies such as geothermal, concentrated solar power, and nuclear, usually demands simultaneous advancement of thermal energy storage (TES) to support on-demand electricity generation and industrial applications while mitigating the inherent intermittency of renewable energy sources and power outages from direct energy generation. Among TES technologies, thermochemical energy storage (TCES) based on calcium looping emerges as a compelling high-power energy storage candidate due to its high reaction enthalpy, compatibility with elevated operating temperatures, and abundance of low-cost materials. However, the long-term durability of calcium-based sorbents for TCES is hindered by surface sintering and particle aggregation, leading to performance degradation over repeated thermal cycles. This study explores a moisture hydration-based strategy to regenerate a degraded calcium sorbent and mitigate performance degradation for long duration TCES. The addition of moisture transforms calcium oxide into calcium hydroxide and produces intercalation water layers, associated with a regenerated surface area and reduced calcium oxide crystallite size. Both these effects are beneficial in restoring the sorbents' reactivity for carbonization. Additionally, an optimized hydration-assisted reactivation protocol balances the recovered energy storage capacity with heating penalty required for moisture removal from hydrated samples, resulting in an enhanced energy storage capacity up to 176% compared to benchmark sorbents that undergo cycling without reactivation after 60 cycles. In conclusion, these results highlight the potential of hydration-assisted reactivation to enhance the long-term performance of TCES, providing an effective pathway to advancing electro-thermal storage technologies.

36 MATERIALS SCIENCE↗