Phase stability of carbon, oxygen and carbon dioxide under extreme P-T conditions, beyond the harmonic approximation

Tesis (Doctor en Ciencias Física). -- Universidad de Cartagena. Facultad de Ciencias Exactas y Naturales, 2020

Autores:
Cogollo Olivo, Beatriz Helena
Tipo de recurso:
Fecha de publicación:
2020
Institución:
Universidad de Cartagena
Repositorio:
Repositorio Universidad de Cartagena
Idioma:
eng
OAI Identifier:
oai:repositorio.unicartagena.edu.co:11227/11078
Acceso en línea:
https://hdl.handle.net/11227/11078
http://dx.doi.org/10.57799/11227/143
Palabra clave:
Física del estado sólido
Transformaciones de fase (Física estadística)
Materiales a alta presión
Rights
License
https://creativecommons.org/licenses/by-nc-nd/4.0
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network_name_str Repositorio Universidad de Cartagena
repository_id_str
dc.title.es.fl_str_mv Phase stability of carbon, oxygen and carbon dioxide under extreme P-T conditions, beyond the harmonic approximation
title Phase stability of carbon, oxygen and carbon dioxide under extreme P-T conditions, beyond the harmonic approximation
spellingShingle Phase stability of carbon, oxygen and carbon dioxide under extreme P-T conditions, beyond the harmonic approximation
Física del estado sólido
Transformaciones de fase (Física estadística)
Materiales a alta presión
title_short Phase stability of carbon, oxygen and carbon dioxide under extreme P-T conditions, beyond the harmonic approximation
title_full Phase stability of carbon, oxygen and carbon dioxide under extreme P-T conditions, beyond the harmonic approximation
title_fullStr Phase stability of carbon, oxygen and carbon dioxide under extreme P-T conditions, beyond the harmonic approximation
title_full_unstemmed Phase stability of carbon, oxygen and carbon dioxide under extreme P-T conditions, beyond the harmonic approximation
title_sort Phase stability of carbon, oxygen and carbon dioxide under extreme P-T conditions, beyond the harmonic approximation
dc.creator.fl_str_mv Cogollo Olivo, Beatriz Helena
dc.contributor.advisor.none.fl_str_mv Montoya Martínez, Javier Antonio
Scandolo, Sandro (Asesor/a)
dc.contributor.author.none.fl_str_mv Cogollo Olivo, Beatriz Helena
dc.subject.es.fl_str_mv Física del estado sólido
Transformaciones de fase (Física estadística)
Materiales a alta presión
topic Física del estado sólido
Transformaciones de fase (Física estadística)
Materiales a alta presión
description Tesis (Doctor en Ciencias Física). -- Universidad de Cartagena. Facultad de Ciencias Exactas y Naturales, 2020
publishDate 2020
dc.date.accessioned.none.fl_str_mv 2020-11-09T18:16:27Z
dc.date.available.none.fl_str_mv 2020-11-09T18:16:27Z
dc.date.issued.none.fl_str_mv 2020
dc.type.spa.fl_str_mv Trabajo de grado - Doctorado
dc.type.coar.fl_str_mv http://purl.org/coar/resource_type/c_db06
dc.type.driver.none.fl_str_mv info:eu-repo/semantics/doctoralThesis
dc.identifier.citation.es.fl_str_mv TD530.41 / C676
dc.identifier.uri.none.fl_str_mv https://hdl.handle.net/11227/11078
http://dx.doi.org/10.57799/11227/143
identifier_str_mv TD530.41 / C676
url https://hdl.handle.net/11227/11078
http://dx.doi.org/10.57799/11227/143
dc.language.iso.fl_str_mv eng
language eng
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rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-nd/4.0
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dc.format.medium.es.fl_str_mv application/pdf
dc.publisher.es.fl_str_mv Universidad de Cartagena
institution Universidad de Cartagena
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spelling Montoya Martínez, Javier Antonio4e5451ccf08bda25d9d6d997448242edScandolo, Sandro (Asesor/a)fe08d5de2db25c127f6bbddcfcefa45fCogollo Olivo, Beatriz Helenad852d835a3e6c64f29000f039bfc6e582020-11-09T18:16:27Z2020-11-09T18:16:27Z2020TD530.41 / C676https://hdl.handle.net/11227/11078http://dx.doi.org/10.57799/11227/143Tesis (Doctor en Ciencias Física). -- Universidad de Cartagena. Facultad de Ciencias Exactas y Naturales, 2020Daily, we can observe how pressure and temperature have a profound e ect on matter. For instance, at ambient pressure water transforms into vapor when heated to 100 °C, and becomes ice when cooled to temperatures below 0 °C. Nonetheless, these transformations can also be achieved starting from the liquid state by reducing or increasing pressure to reach the vapor o solid state, respectively. We can study the phase transitions by minimizing the Gibbs free energy: G = U ST + pV (0.1) Where U holds for the internal energy, S for the entropy, and V for the volume of the piece of matter under study. According to this expression, solid phases are favored at low temperatures and/or at high pressures, while at opposite conditions gas phases are favored. Liquids are favored at intermediate regimes. Oxygen is a highly reactive nonmetal and an oxidizing agent that easily forms mixtures with most elements and several other compounds. By mass-fraction, oxygen is the third-most abundant element in the universe, after hydrogen and helium. At ambient conditions, oxygen is a colorless and odorless gas with the molecular formula O2, where two oxygen atoms are chemically bound to each other with a covalent double bond. At atmospheric pressure and low temperature (below 54.36 K), solid oxygen is formed. Solid oxygen is particularly interesting because it is the only simple diatomic molecule to carry a magnetic moment, and it is considered a \spin-controlled" crystal that displays antiferromagnetic order in the low-temperature phases. At high pressure, solid oxygen transforms from an insulating to a metallic state; and at very low temperatures, it even changes into a superconducting state. Referred to as the \king of the elements", carbon is a nonmetallic and tetravalent element, that is also the fourth most abundant element in the universe by mass. Because of the four electrons available to form covalent bonds, the atoms of carbon can bond 1 together in diverse ways, resulting in various allotropes of this element, being the bestknown graphite and diamond. This element has attracted attention because of the system of carbon allotropes spans a range of extremes, i.e., graphite is one of the softest materials known, it is opaque and a good conductor of electricity, while diamond is the hardest naturally occurring substance, it is highly transparent and is an excellent electrical insulator. At elevated temperatures, carbon reacts with oxygen to form oxocarbons or carbon oxides. The simplest and most common oxocarbons are carbon monoxide (CO) and carbon dioxide (CO2). Carbon dioxide consists of a carbon atom covalently double bonded to two oxygen atoms. CO2 is characterized by strong double bonds (C=O distance of 1.16 A ) and rather weak intermolecular interactions, which has made it a very stable system that exhibits several molecular phases before its polymerization. Also at high pressures, another form of solid carbon dioxide is observed: an amorphous glass-like solid named carbonia, that can be produced by supercooling heated CO2 at pressures above 40 GPa. Although this discovery con rmed that carbon dioxide could exist in a glass state similar to other members of its elemental family, like silicon (silica glass) and germanium dioxide, carbonia glass is not stable at normal pressures and reverts to gas when pressure is released. Given their importance for life as we know it, carbon and oxygen have been extensively studied at pressures and temperatures found on the surface of the Earth. Nevertheless, despite their simplicity, they exhibit remarkable properties. Their abundance in the universe justi es the attention of the scienti c community and explains the constant study of these two elements under extreme conditions. In order to study materials at extreme conditions, i.e., those similar at the interior of planets, experimentalists have designed apparatuses that apply force to a small area where the sample is con ned. The diamond anvil cell (DAC) is the most commonly used device and state of the art DACs are able to reach pressures up to 600 GPa, but experiments at these extreme pressures are very challenging. Laser shock-wave experiments are able to reach he terapascal regime for a limited short time. However, along with very high pressures, temperatures of several thousand Kelvin are also achieved, altering the sample's state and making challenging the study of solids at extreme conditions, from the experimental point of view. The technical di culty and high economical cost of high pressure experiments make theoretical approaches specially necessary. Fortunately, theoreticalapplication/pdfUniversidad de Cartagenahttps://creativecommons.org/licenses/by-nc-nd/4.0http://purl.org/coar/access_right/c_abf2Física del estado sólidoTransformaciones de fase (Física estadística)Materiales a alta presiónPhase stability of carbon, oxygen and carbon dioxide under extreme P-T conditions, beyond the harmonic approximationTrabajo de grado - Doctoradoinfo:eu-repo/semantics/doctoralThesishttp://purl.org/coar/resource_type/c_db06engORIGINAL13-TesisDoctoral-BeatrizCogollo.pdf13-TesisDoctoral-BeatrizCogollo.pdfapplication/pdf6893175https://repositorio.unicartagena.edu.co/bitstream/11227/11078/1/13-TesisDoctoral-BeatrizCogollo.pdf62f58d5b124a87fb934cbaec81530633MD51open accessLICENSElicense.txtlicense.txttext/plain; charset=utf-81756https://repositorio.unicartagena.edu.co/bitstream/11227/11078/2/license.txt7b38fcee9ba3bc8639fa56f350c81be3MD52open accessTEXT13-TesisDoctoral-BeatrizCogollo.pdf.txt13-TesisDoctoral-BeatrizCogollo.pdf.txtExtracted texttext/plain262337https://repositorio.unicartagena.edu.co/bitstream/11227/11078/3/13-TesisDoctoral-BeatrizCogollo.pdf.txte2900672d257df2b822d9b13f6ba56e8MD53open accessTHUMBNAIL13-TesisDoctoral-BeatrizCogollo.pdf.jpg13-TesisDoctoral-BeatrizCogollo.pdf.jpgGenerated Thumbnailimage/jpeg8213https://repositorio.unicartagena.edu.co/bitstream/11227/11078/4/13-TesisDoctoral-BeatrizCogollo.pdf.jpgda2b8628a454a0992a32951448e8ef89MD54open access11227/11078oai:repositorio.unicartagena.edu.co:11227/110782023-06-14 09:36:07.837An error occurred on the license name.|||https://creativecommons.org/licenses/by-nc-nd/4.0open accessBiblioteca Digital Universidad de Cartagenabdigital@metabiblioteca.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