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dc.identifier.urihttp://hdl.handle.net/11401/77649
dc.description.sponsorshipThis work is sponsored by the Stony Brook University Graduate School in compliance with the requirements for completion of degree.en_US
dc.formatMonograph
dc.format.mediumElectronic Resourceen_US
dc.language.isoen_US
dc.publisherThe Graduate School, Stony Brook University: Stony Brook, NY.
dc.typeDissertation
dcterms.abstractA physics-based understanding of the behavior of materials under conditions of high-pressure and high-temperature is full of excitement and challenges. Here, we mainly cover two parts within the subject of high pressure science with USPEX – crystal structure prediction in materials containing hydrogen, and investigation of mechanisms of structural phase transitions. We applied the USPEX method to study hydrogen hydrate, and hydronitrogen materials. In hydrogen hydrate system, we confirmed that the H2O-H2 system undergoes a series of transformations with pressure, and adopts the known open-network clathrate structures (sII, C0), dense " filled ice" structures (C1, C2) and found two novel hydrogen hydrate phases. For hydronitrogen under pressure, numerous unreported and exotic phases are found at pressure up to 800 GPa, such as N4H, N3H, N2H and NH phases composed of nitrogen backbones, the N9H4 phase containing two-dimensional metallic nitrogen planes and novel N8H, NH2, N3H7, NH4 and NH5 molecular phases. Another surprise is that NH3 becomes thermodynamically unstable above ∼460 GPa. To reveal the phase transition mechanism and pathway for simple and small systems, the variable-cell NEB (VC-NEB) method was developed, which is very efficient for finding the phase transition path within a static mean-field picture. The method has been applied to the various reconstructive solid-solid B4→B1 and B3→B1 phase transitions of GaN, phase transition in MgF2 system and guide for experiments for materials synthesis. Combine with the evolutionary metadynamics (EV-metadynamics) and the transition path sampling (TPS) approach, a general procedure for structure phase transition investigation in USPEX is introduced. Different levels of investigation of the fcc→hcp transformation in argon with EV-metadynamics, VC-NEB and TPS methods are performed, helping us to understand comprehensively and deeply the phase transition pathway and mechanism.
dcterms.abstractA physics-based understanding of the behavior of materials under conditions of high-pressure and high-temperature is full of excitement and challenges. Here, we mainly cover two parts within the subject of high pressure science with USPEX – crystal structure prediction in materials containing hydrogen, and investigation of mechanisms of structural phase transitions. We applied the USPEX method to study hydrogen hydrate, and hydronitrogen materials. In hydrogen hydrate system, we confirmed that the H2O-H2 system undergoes a series of transformations with pressure, and adopts the known open-network clathrate structures (sII, C0), dense " filled ice" structures (C1, C2) and found two novel hydrogen hydrate phases. For hydronitrogen under pressure, numerous unreported and exotic phases are found at pressure up to 800 GPa, such as N4H, N3H, N2H and NH phases composed of nitrogen backbones, the N9H4 phase containing two-dimensional metallic nitrogen planes and novel N8H, NH2, N3H7, NH4 and NH5 molecular phases. Another surprise is that NH3 becomes thermodynamically unstable above ∼460 GPa. To reveal the phase transition mechanism and pathway for simple and small systems, the variable-cell NEB (VC-NEB) method was developed, which is very efficient for finding the phase transition path within a static mean-field picture. The method has been applied to the various reconstructive solid-solid B4→B1 and B3→B1 phase transitions of GaN, phase transition in MgF2 system and guide for experiments for materials synthesis. Combine with the evolutionary metadynamics (EV-metadynamics) and the transition path sampling (TPS) approach, a general procedure for structure phase transition investigation in USPEX is introduced. Different levels of investigation of the fcc→hcp transformation in argon with EV-metadynamics, VC-NEB and TPS methods are performed, helping us to understand comprehensively and deeply the phase transition pathway and mechanism.
dcterms.available2017-09-20T16:53:11Z
dcterms.contributorWeidner, Donalden_US
dcterms.contributorPhillips, Brianen_US
dcterms.contributorOganov, Artem R.en_US
dcterms.contributorRasbury, Troyen_US
dcterms.contributorAllen, Phillips.en_US
dcterms.creatorQian, Guangrui
dcterms.dateAccepted2017-09-20T16:53:11Z
dcterms.dateSubmitted2017-09-20T16:53:11Z
dcterms.descriptionDepartment of Geosciences.en_US
dcterms.extent133 pg.en_US
dcterms.formatMonograph
dcterms.formatApplication/PDFen_US
dcterms.identifierhttp://hdl.handle.net/11401/77649
dcterms.issued2015-05-01
dcterms.languageen_US
dcterms.provenanceMade available in DSpace on 2017-09-20T16:53:11Z (GMT). No. of bitstreams: 1 Qian_grad.sunysb_0771E_12461.pdf: 14868602 bytes, checksum: 34b0d96eeb41d10c14bd7b5c3adce352 (MD5) Previous issue date: 2015en
dcterms.publisherThe Graduate School, Stony Brook University: Stony Brook, NY.
dcterms.subjectevolutionary algorithm, hydrogen hydrate, hydronitrogens, Phase transition, Structure Prediction, USPEX
dcterms.subjectGeophysics
dcterms.titleMaterials Structure Prediction and Phase Transition Mechanism Investigation
dcterms.typeDissertation


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