Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/111422
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dc.contributorDepartment of Applied Physicsen_US
dc.creatorYang, Ken_US
dc.creatorYang, Ken_US
dc.creatorYang, Ten_US
dc.creatorHe, Jen_US
dc.creatorYang, Men_US
dc.creatorZhou, Ten_US
dc.date.accessioned2025-02-27T04:12:14Z-
dc.date.available2025-02-27T04:12:14Z-
dc.identifier.other50232-
dc.identifier.urihttp://hdl.handle.net/10397/111422-
dc.language.isoenen_US
dc.publisherAmerican Physical Societyen_US
dc.rights©2024 American Physical Societyen_US
dc.rightsThe following publication Yang, K., Yang, K., Yang, T., He, J., Yang, M., & Zhou, T. (2024). Potential existence of Xe3CO2 compounds with distinct Xe-C covalent bonds under pressures of Earth's core. Physical Review B, 110(5), 054108 is available at https://doi.org/10.1103/PhysRevB.110.054108.en_US
dc.titlePotential existence of Xe₃CO₂ compounds with distinct Xe-C covalent bonds under pressures of Earth's coreen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume110en_US
dc.identifier.issue5en_US
dc.identifier.doi10.1103/PhysRevB.110.054108en_US
dcterms.abstractNoble gas compounds have attracted significant research attention, mainly due to their intriguing chemical behavior under high-pressure conditions. In this paper, we identify a compound, C2/m-Xe3CO2, through a synergistic approach combining a particle-swarm optimization empowered structure search and first-principles calculations within a wide pressure range of 200-400 GPa, covering the pressure range of Earth's core. This compound features layered Xe6C2O4 sublattices, showing distinct covalent Xe-C bonds, supported by the calculated electron localization function. The presence of the covalent bonds is further corroborated by the large value of the integrated crystal orbital Hamilton population (-4.02 eV/pair) and the large negative Laplacian (-4.65e/Å5). This leads to an unusual sp3-like hybridization in carbon, involving two oxygen atoms, one carbon atom, and one xenon atom. Additionally, two-phase method molecular dynamics simulations suggest that the compound exhibits liquid-state behavior at 200 GPa and 5000 K above the geotherm of the Earth's core. This shows a potential role for the compound in the liquid phase as a reservoir for the "missing Xe"phenomenon. Our findings not only enhance the understanding of bonding behavior in noble gas compounds, but also suggest the potential presence of Xe3CO2 in various astronomical objects.en_US
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationPhysical review B : covering condensed matter and materials physics, 1 Aug. 2024, v. 110, no. 5, 054108en_US
dcterms.isPartOfPhysical review B : covering condensed matter and materials physicsen_US
dcterms.issued2024-08-01-
dc.identifier.scopus2-s2.0-85201715638-
dc.identifier.eissn2469-9950en_US
dc.identifier.artn054108en_US
dc.description.validate202502 bcchen_US
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_Others; a3484c, a3719-
dc.identifier.SubFormID50234, 50852-
dc.description.fundingSourceRGCen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextHong Kong Polytechnic University; High Performance Computing Platform at the Eastern Institute of Technology, Ningbo; Hong Kong Polytechnic Universityen_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryVoR alloweden_US
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