Search NASA⌕ Search

DOE OSTI · 1749152

Materials Data on Ba4Fe12Si8ClO35 by Materials Project

Abstract

Ba4Fe12Si8O35Cl crystallizes in the triclinic P1 space group. The structure is three-dimensional. there are four inequivalent Ba2+ sites. In the first Ba2+ site, Ba2+ is bonded in a 10-coordinate geometry to ten O2- atoms. There are a spread of Ba–O bond distances ranging from 2.76–3.01 Å. In the second Ba2+ site, Ba2+ is bonded in a 11-coordinate geometry to ten O2- and one Cl1- atom. There are a spread of Ba–O bond distances ranging from 2.79–3.04 Å. The Ba–Cl bond length is 3.16 Å. In the third Ba2+ site, Ba2+ is bonded in a 10-coordinate geometry to ten O2- atoms. There are a spread of Ba–O bond distances ranging from 2.77–3.02 Å. In the fourth Ba2+ site, Ba2+ is bonded in a 10-coordinate geometry to ten O2- atoms. There are a spread of Ba–O bond distances ranging from 2.76–2.99 Å. There are twelve inequivalent Fe+2.58+ sites. In the first Fe+2.58+ site, Fe+2.58+ is bonded to six O2- atoms to form FeO6 octahedra that share corners with two SiO4 tetrahedra, corners with two FeO5 trigonal bipyramids, and edges with six FeClO5 octahedra. There are a spread of Fe–O bond distances ranging from 2.16–2.32 Å. In the second Fe+2.58+ site, Fe+2.58+ is bonded to five O2- and one Cl1- atom to form distorted FeClO5 octahedra that share corners with two SiO4 tetrahedra, corners with two FeO5 trigonal bipyramids, and edges with six FeClO5 octahedra. There are a spread of Fe–O bond distances ranging from 2.13–2.36 Å. The Fe–Cl bond length is 2.60 Å. In the third Fe+2.58+ site, Fe+2.58+ is bonded to five O2- and one Cl1- atom to form distorted FeClO5 octahedra that share corners with two SiO4 tetrahedra, corners with two FeO5 trigonal bipyramids, and edges with six FeO6 octahedra. There are a spread of Fe–O bond distances ranging from 2.16–2.25 Å. The Fe–Cl bond length is 2.56 Å. In the fourth Fe+2.58+ site, Fe+2.58+ is bonded to six O2- atoms to form FeO6 octahedra that share corners with two SiO4 tetrahedra, corners with two FeO5 trigonal bipyramids, and edges with six FeO6 octahedra. There are a spread of Fe–O bond distances ranging from 1.97–2.30 Å. In the fifth Fe+2.58+ site, Fe+2.58+ is bonded to five O2- atoms to form distorted FeO5 trigonal bipyramids that share corners with three FeClO5 octahedra and corners with four SiO4 tetrahedra. The corner-sharing octahedra tilt angles range from 63–65°. There are a spread of Fe–O bond distances ranging from 1.91–2.01 Å. In the sixth Fe+2.58+ site, Fe+2.58+ is bonded to five O2- atoms to form distorted FeO5 trigonal bipyramids that share corners with three FeO6 octahedra and corners with four SiO4 tetrahedra. The corner-sharing octahedra tilt angles range from 60–67°. There are a spread of Fe–O bond distances ranging from 1.89–2.01 Å. In the seventh Fe+2.58+ site, Fe+2.58+ is bonded to five O2- atoms to form distorted FeO5 trigonal bipyramids that share corners with three FeClO5 octahedra and corners with four SiO4 tetrahedra. The corner-sharing octahedra tilt angles range from 61–71°. There are a spread of Fe–O bond distances ranging from 1.89–2.01 Å. In the eighth Fe+2.58+ site, Fe+2.58+ is bonded to five O2- atoms to form distorted FeO5 trigonal bipyramids that share corners with three FeO6 octahedra and corners with four SiO4 tetrahedra. The corner-sharing octahedra tilt angles range from 58–67°. There are a spread of Fe–O bond distances ranging from 1.88–2.01 Å. In the ninth Fe+2.58+ site, Fe+2.58+ is bonded to six O2- atoms to form FeO6 octahedra that share corners with four SiO4 tetrahedra and edges with six FeO6 octahedra. There are a spread of Fe–O bond distances ranging from 1.91–2.26 Å. In the tenth Fe+2.58+ site, Fe+2.58+ is bonded to five O2- and one Cl1- atom to form distorted FeClO5 octahedra that share corners with four SiO4 tetrahedra and edges with six FeO6 octahedra. There are a spread of Fe–O bond distances ranging from 1.86–2.20 Å. The Fe–Cl bond length is 2.44 Å. In the eleventh Fe+2.58+ site, Fe+2.58+ is bonded to six O2- atoms to form FeO6 octahedra that share corners with four SiO4 tetrahedra, corners with two FeO5 trigonal bipyramids, and edges with six FeO6 octahedra. There are a spread of Fe–O bond distances ranging from 2.03–2.37 Å. In the twelfth Fe+2.58+ site, Fe+2.58+ is bonded to six O2- atoms to form FeO6 octahedra that share corners with four SiO4 tetrahedra, corners with two FeO5 trigonal bipyramids, and edges with six FeO6 octahedra. There are a spread of Fe–O bond distances ranging from 2.03–2.38 Å. There are eight inequivalent Si4+ sites. In the first Si4+ site, Si4+ is bonded to four O2- atoms to form SiO4 tetrahedra that share corners with three FeO6 octahedra, a cornercorner with one SiO4 tetrahedra, and corners with two FeO5 trigonal bipyramids. The corner-sharing octahedra tilt angles range from 57–61°. There are a spread of Si–O bond distances ranging from 1.63–1.66 Å. In the second Si4+ site, Si4+ is bonded to four O2- atoms to form SiO4 tetrahedra that share corners with three FeClO5 octahedra, a cornercorner with one SiO4 tetrahedra, and corners with two FeO5 trigonal bipyramids. The corner-sharing octahedra tilt angles range from 57–62°. There are a spread of Si–O bond distances ranging from 1.63–1.66 Å. In the third Si4+ site, Si4+ is bonded to four O2- atoms to form SiO4 tetrahedra that share corners with three FeClO5 octahedra, a cornercorner with one SiO4 tetrahedra, and corners with two FeO5 trigonal bipyramids. The corner-sharing octahedra tilt angles range from 56–62°. There are a spread of Si–O bond distances ranging from 1.63–1.66 Å. In the fourth Si4+ site, Si4+ is bonded to four O2- atoms to form SiO4 tetrahedra that share corners with three FeO6 octahedra, a cornercorner with one SiO4 tetrahedra, and corners with two FeO5 trigonal bipyramids. The corner-sharing octahedra tilt angles range from 58–61°. There is two shorter (1.63 Å) and two longer (1.66 Å) Si–O bond length. In the fifth Si4+ site, Si4+ is bonded to four O2- atoms to form SiO4 tetrahedra that share corners with three FeClO5 octahedra, a cornercorner with one SiO4 tetrahedra, and corners with two FeO5 trigonal bipyramids. The corner-sharing octahedra tilt angles range from 61–64°. There are a spread of Si–O bond distances ranging from 1.63–1.66 Å. In the sixth Si4+ site, Si4+ is bonded to four O2- atoms to form SiO4 tetrahedra that share corners with three FeO6 octahedra, a cornercorner with one SiO4 tetrahedra, and corners with two FeO5 trigonal bipyramids. The corner-sharing octahedra tilt angles range from 56–64°. There are a spread of Si–O bond distances ranging from 1.63–1.66 Å. In the seventh Si4+ site, Si4+ is bonded to four O2- atoms to form SiO4 tetrahedra that share corners with three FeO6 octahedra, a cornercorner with one SiO4 tetrahedra, and corners with two FeO5 trigonal bipyramids. The corner-sharing octahedra tilt angles range from 58–62°. There are a spread of Si–O bond distances ranging from 1.63–1.66 Å. In the eighth Si4+ site, Si4+ is bonded to four O2- atoms to form SiO4 tetrahedra that share corners with three FeClO5 octahedra, a cornercorner with one SiO4 tetrahedra, and corners with two FeO5 trigonal bipyramids. The corner-sharing octahedra tilt angles range from 60–66°. There are a spread of Si–O bond distances ranging from 1.63–1.66 Å. There are thirty-five inequivalent O2- sites. In the first O2- site, O2- is bonded in a 4-coordinate geometry to three Fe+2.58+ and one Si4+ atom. In the second O2- site, O2- is bonded in a 4-coordinate geometry to three Fe+2.58+ and one Si4+ atom. In the third O2- site, O2- is bonded in a 4-coordinate geometry to three Fe+2.58+ and one Si4+ atom. In the fourth O2- site, O2- is bonded in a 4-coordinate geometry to three Fe+2.58+ and one Si4+ atom. In the fifth O2- site, O2- is bonded to three Fe+2.58+ and one Si4+ atom to form distorted OFe3Si tetrahedra that share corners with three OFe3Si tetrahedra and an edgeedge with one OFe4 tetrahedra. In the sixth O2- site, O2- is bonded in a distorted rectangular see-saw-like geometry to three Fe+2.58+ and one Si4+ atom. In the seventh O2- site, O2- is bonded in a 4-coordinate geometry to three Fe+2.58+ and one Si4+ atom. In the eighth O2- site, O2- is bonded to three Fe+2.58+ and one Si4+ atom to form a mixture of distorted corner and edge-sharing OFe3Si tetrahedra. In the ninth O2- site, O2- is bonded in a 4-coordinate geometry to two Ba2+, one Fe+2.58+, and one Si4+ atom. In the tenth O2- site, O2- is bonded in a 4-coordinate geometry to two Ba2+, one Fe+2.58+, and one Si4+ atom. In the eleventh O2- site, O2- is bonded in a 4-coordinate geometry to two Ba2+, one Fe+2.58+, and one Si4+ atom. In the twelfth O2- site, O2- is bonded in a 4-coordinate geometry to two Ba2+, one Fe+2.58+, and one Si4+ atom. In the thirteenth O2- site, O2- is bonded in a 4-coordinate geometry to two Ba2+, one Fe+2.58+, and one Si4+ atom. In the fourteenth O2- site, O2- is bonded in a 4-coordinate geometry to two Ba2+, one Fe+2.58+, and one Si4+ atom. In the fifteenth O2- site, O2- is bonded in a 4-coordinate geometry to two Ba2+, one Fe+2.58+, and one Si4+ atom. In the sixteenth O2- site, O2- is bonded in a 2-coordinate geometry to two Ba2+, one Fe+2.58+, and one Si4+ atom. In the seventeenth O2- site, O2- is bonded in a bent 150 degrees geometry to two Ba2+ and two Si4+ atoms. In the eighteenth O2- site, O2- is bonded in a bent 150 degrees geometry to two Ba2+ and two Si4+ atoms. In the nineteenth O2- site, O2- is bonded in a bent 150 degrees geometry to two Ba2+ and two Si4+ atoms. In the twentieth O2- site, O2- is bonded in a bent 150 degrees geometry to two Ba2+ and two Si4+ atoms. In the twenty-first O2- site, O2- is bonded to four Fe+2.58+ atoms to form distorted OFe4 tetrahedra that share a cornercorner with one OFe4 tetrahedra and edges with two OFe3Si tetrahedra. In the twenty-second O2- site, O2- is bonded to four Fe+2.58+ atoms to form a mixture of distorted corner and edge-sharing OFe4 tetrahedra. In the twenty-third O2- site, O2- is bonded to four Fe+2.58+ atoms to form distorted OFe4 tetrahedra that share corners with three OFe3Si tetrahedra and an edgeedge with one OFe4 tetrahedra. In the twenty-fourth O2- site, O2- is bonded to four Fe+2.58+ atoms to form distorted OFe4 tetrahedra that share corners with three OFe3Si tetrahedra and an edgeedge with one OFe4 tetrahedra. In the twenty-fifth O2- site, O2- is bonded in a 2-coordinate geometry to two Ba2+, one Fe+2.58+, and one Si4+ atom. In the twenty-sixth O2- site, O2- is bonded in a 4-coordinate geometry to two Ba2+, one Fe+2.58+, and one Si4+ atom. In the twenty-seventh O2- site, O2- is bonded in a 4-coordinate geometry to two Ba2+, one Fe+2.58+, and one Si4+ atom. In the twenty-eighth O2- site, O2- is bonded in a 4-coordinate geometry to two Ba2+, one Fe+2.58+, and one Si4+ atom. In the twenty-ninth O2- site, O2- is bonded in a 4-coordinate geometry to two Ba2+, one Fe+2.58+, and one Si4+ atom. In the thirtieth O2- site, O2- is bonded in a 4-coordinate geometry to two Ba2+, one Fe+2.58+, and one Si4+ atom. In the thirty-first O2- site, O2- is bonded in a 4-coordinate geometry to two Ba2+, one Fe+2.58+, and one Si4+ atom. In the thirty-second O2- site, O2- is bonded in a 4-coordinate geometry to two Ba2+, one Fe+2.58+, and one Si4+ atom. In the thirty-third O2- site, O2- is bonded in a trigonal non-coplanar geometry to three Fe+2.58+ atoms. In the thirty-fourth O2- site, O2- is bonded in a 3-coordinate geometry to three Fe+2.58+ atoms. In the thirty-fifth O2- site, O2- is bonded in a distorted trigonal non-coplanar geometry to three Fe+2.58+ atoms. Cl1- is bonded in a 4-coordinate geometry to one Ba2+ and three Fe+2.58+ atoms.

Explore related subjects

Keep this discovery

Explore connections, maps & timelines

BibTeXRIS

2020-04-29. Materials Data on Ba4Fe12Si8ClO35 by Materials Project. https://doi.org/10.17188/1749152

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↗