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dc.contributor.authorLee, Young-Su-
dc.contributor.authorKim, Yoonyoung-
dc.contributor.authorCho, Young Whan-
dc.contributor.authorShapiro, Daniel-
dc.contributor.authorWolverton, Chris-
dc.contributor.authorOzolins, Vidvuds-
dc.date.accessioned2024-01-20T22:00:32Z-
dc.date.available2024-01-20T22:00:32Z-
dc.date.created2021-09-03-
dc.date.issued2009-03-
dc.identifier.issn1098-0121-
dc.identifier.urihttps://pubs.kist.re.kr/handle/201004/132705-
dc.description.abstractCa(BH4)(2) is an interesting candidate for high-density hydrogen storage since it contains a large amount of hydrogen by weight and volume, and has been shown to reversibly release and absorb hydrogen, albeit at moderately high temperatures. Ca(BH4)(2) undergoes a polymorphic transformation around 400-440 K from a low-temperature alpha-Ca(BH4)(2) phase to a high-temperature beta-Ca(BH4)(2) phase. The crystal structure of beta-Ca(BH4)(2) has only recently been resolved, and its thermodynamic phase stability is still not well understood. Using a combined experimental and theoretical approach, we have independently determined the structure of beta-Ca(BH4)(2) and assessed its thermodynamic stability in the quasiharmonic approximation. The space-group P4(2)/m gives an excellent agreement between experiment and theory, confirming the result of a recent study [Buchter et al., J. Phys. Chem. B 112, 8042 (2008)]. Using density-functional theory (DFT), we obtained a value of 10.9 kJ/mol for the static total-energy difference between the beta-Ca(BH4)(2) and the alpha-Ca(BH4)(2) phases at T=0 K (without vibrations). Using DFT linear-response calculations, we find that the [1/21/2 xi] acoustic phonon branch of beta-Ca(BH4)(2) is dynamically unstable on the Brillouin-zone boundary at the T=0 K lattice parameters predicted from static DFT calculations. This phonon branch is very sensitive to the lattice parameters and can be stabilized by including lattice expansion due to zero-point vibrational contributions in the quasiharmonic approximation. This expanded stable beta-Ca(BH4)(2) structure has a room-temperature vibrational entropy that is 16 J/mol K higher than that of the alpha-Ca(BH4)(2) phase, qualitatively consistent with the observed stabilization of the former at elevated temperatures. The main contribution to the entropy difference between the alpha-Ca(BH4)(2) and beta-Ca(BH4)(2) phases comes from the low-frequency region dominated by translational and rotational phonon modes.-
dc.languageEnglish-
dc.publisherAMER PHYSICAL SOC-
dc.subjectHYDROGEN STORAGE-
dc.subjectMAGNESIUM BOROHYDRIDE-
dc.subjectCALCIUM BOROHYDRIDE-
dc.subjectELECTRON-GAS-
dc.subjectCA(BH4)(2)-
dc.subjectDIFFRACTION-
dc.subjectLIBH4-
dc.subjectMG(BH4)(2)-
dc.subjectDYNAMICS-
dc.subjectNEUTRON-
dc.titleCrystal structure and phonon instability of high-temperature beta-Ca(BH4)(2)-
dc.typeArticle-
dc.identifier.doi10.1103/PhysRevB.79.104107-
dc.description.journalClass1-
dc.identifier.bibliographicCitationPHYSICAL REVIEW B, v.79, no.10-
dc.citation.titlePHYSICAL REVIEW B-
dc.citation.volume79-
dc.citation.number10-
dc.description.journalRegisteredClassscie-
dc.description.journalRegisteredClassscopus-
dc.identifier.wosid000264768600034-
dc.identifier.scopusid2-s2.0-63249110680-
dc.relation.journalWebOfScienceCategoryMaterials Science, Multidisciplinary-
dc.relation.journalWebOfScienceCategoryPhysics, Applied-
dc.relation.journalWebOfScienceCategoryPhysics, Condensed Matter-
dc.relation.journalResearchAreaMaterials Science-
dc.relation.journalResearchAreaPhysics-
dc.type.docTypeArticle-
dc.subject.keywordPlusHYDROGEN STORAGE-
dc.subject.keywordPlusMAGNESIUM BOROHYDRIDE-
dc.subject.keywordPlusCALCIUM BOROHYDRIDE-
dc.subject.keywordPlusELECTRON-GAS-
dc.subject.keywordPlusCA(BH4)(2)-
dc.subject.keywordPlusDIFFRACTION-
dc.subject.keywordPlusLIBH4-
dc.subject.keywordPlusMG(BH4)(2)-
dc.subject.keywordPlusDYNAMICS-
dc.subject.keywordPlusNEUTRON-
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