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Physical processes influence on the dynamics of the main greenhouse gases in mountain tropical reservoirs
dc.rights.license | Atribución-NoComercial-SinDerivadas 4.0 Internacional |
dc.contributor.advisor | Lorke, Andreas |
dc.contributor.advisor | Gómez Giraldo, Andrés |
dc.contributor.advisor | León Hernández, Juan Gabriel |
dc.contributor.author | Bohórquez Bedoya, Eliana |
dc.date.accessioned | 2023-07-21T15:23:16Z |
dc.date.available | 2023-07-21T15:23:16Z |
dc.date.issued | 2023-07-13 |
dc.identifier.uri | https://repositorio.unal.edu.co/handle/unal/84240 |
dc.description | ilustraciones, diagramas, mapas |
dc.description.abstract | Tropical reservoirs are recognized as globally important sources of greenhouse gases (GHG). Tropical mountainous areas of high hydroelectric development have been poorly studied. The objective of this study is to understand GHG dynamics in tropical mountain reservoirs. Data on seasonal and diurnal GHG dynamics were collected during six field campaigns in the Porce III reservoir in the Colombian Andes, where the importance of oxic CH4 production in the variability of dissolved gas at the surface, as well as the variation of water levels as an incident factor in GHG fluxes on a seasonal scale, was evidenced. CO2 flux at the reservoir water-atmosphere interface were monitored with a high-resolution technique over periods of several weeks, where the importance of primary productivity in the diurnal cycling of CO2 flux was inferred, showing alternation as sink-source, and pulses of synoptic-scale CO2 flux were observed as a consequence of the simultaneous occurrence of increases in surface concentrations and high wind speed. In laboratory experiments, a relationship was found between rain rate, turbulent kinetic energy dissipation rate and gas transfer rate, contributing to the modeling of this phenomenon with applicability in inland waters. In general, the results obtained contribute to the understanding of GHG dynamics in eutrophic tropical reservoirs. |
dc.description.abstract | Los embalses tropicales están reconocidos como fuentes de gases de efecto invernadero (GEI) de importancia mundial. Zonas tropicales montañosas de gran desarrollo hidroeléctrico han sido escasamente estudiadas. El objetivo de este estudio es comprender la dinámica de los GEI en embalses tropicales de montaña. Se recolectaron datos de la dinámica estacional y diurna de GEI durante seis campañas de campo en el embalse Porce III, en los Andes colombianos, donde se evidenció la importancia de la producción óxica de CH4 en la en la variabilidad del gas disuelto en superficie, así como la variación de los niveles de agua como factor incidente en los flujos de GEI a escala estacional. Se monitoreó el flujo de CO2 en la interfaz agua-atmósfera del embalse con una técnica de alta resolución durante periodos de varias semanas, donde se infirió la importancia de la productividad primaria en el ciclo diurno de los flujos de CO2, mostrando alternancia como sumidero-fuente, y se observaron pulsos de flujos de CO2 a escala sinóptica como consecuencia de la ocurrencia simultánea de incrementos en las concentraciones superficiales y alta velocidad del viento. En experimentos de laboratorio, se encontró una relación entre la tasa de lluvia, la tasa de disipación de la energía cinética turbulenta y la velocidad de transferencia de gases, contribuyendo a la modelación de este fenómeno con aplicabilidad en aguas continentales. En general, los resultados obtenidos contribuyen al entendimiento de la dinámica de GEI en embalses tropicales eutrofizados. (Texto tomado de la fuente) |
dc.description.sponsorship | Scholarship Program No. 757 - National Doctorates of the Ministry of Science, Technology and Innovation of Colombia |
dc.description.sponsorship | Research Grants - Short-Term Grants, 2019 (57440917) of the German Academic Exchange Service (DAAD) |
dc.description.sponsorship | the German Research Foundation (DFG). |
dc.description.sponsorship | Ministerio de Ciencia Tecnología e Innovación de Colombia - MinCiencias |
dc.format.extent | 156 páginas |
dc.format.mimetype | application/pdf |
dc.language.iso | eng |
dc.publisher | Universidad Nacional de Colombia |
dc.publisher | Technische Universität Kaiserslautern-Landau |
dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/4.0/ |
dc.subject.ddc | 620 - Ingeniería y operaciones afines::627 - Ingeniería hidráulica |
dc.title | Physical processes influence on the dynamics of the main greenhouse gases in mountain tropical reservoirs |
dc.type | Trabajo de grado - Doctorado |
dc.type.driver | info:eu-repo/semantics/doctoralThesis |
dc.type.version | info:eu-repo/semantics/acceptedVersion |
dc.publisher.program | Medellín - Minas - Doctorado en Ingeniería - Recursos Hidráulicos |
dc.description.notes | Recibió simultáneamente el grado de Doctor en Ciencias Naturales por la Technische Universität Kaiserslautern-Landau de Alemania |
dc.description.degreelevel | Doctorado |
dc.description.degreename | Doctor en Ingeniería |
dc.identifier.instname | Universidad Nacional de Colombia |
dc.identifier.repo | Repositorio Institucional Universidad Nacional de Colombia |
dc.identifier.repourl | https://repositorio.unal.edu.co/ |
dc.publisher.faculty | Facultad de Minas |
dc.publisher.place | Medellín, Colombia |
dc.publisher.branch | Universidad Nacional de Colombia - Sede Medellín |
dc.relation.indexed | RedCol |
dc.relation.indexed | LaReferencia |
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dc.rights.accessrights | info:eu-repo/semantics/openAccess |
dc.subject.lemb | Gases de invernadero |
dc.subject.lemb | Greenhouse gases |
dc.subject.lemb | Canales (Ingeniería hidráulica) |
dc.subject.lemb | Channels (hydraulic engineering) |
dc.subject.proposal | Tropical mountain reservoirs |
dc.subject.proposal | Greenhouse gases |
dc.subject.proposal | Gas transfer at the water-atmosphere interface |
dc.subject.proposal | Seasonal variability |
dc.subject.proposal | Diurnal cycle |
dc.subject.proposal | Rainfall rate |
dc.subject.proposal | Embalses tropicales de montaña |
dc.subject.proposal | Gases efecto invernadero |
dc.subject.proposal | Transferencia de gases en la interfaz agua-atmósfera |
dc.subject.proposal | Variabilidad estacional |
dc.subject.proposal | Ciclo diurno |
dc.subject.proposal | Tasa de lluvia |
dc.title.translated | Influencia de los procesos físicos en la dinámica de los principales gases de efecto invernadero en embalses tropicales de montaña |
dc.type.coar | http://purl.org/coar/resource_type/c_db06 |
dc.type.coarversion | http://purl.org/coar/version/c_ab4af688f83e57aa |
dc.type.content | Text |
dc.type.redcol | http://purl.org/redcol/resource_type/TD |
oaire.accessrights | http://purl.org/coar/access_right/c_abf2 |
dcterms.audience.professionaldevelopment | Público general |
dc.description.curriculararea | Área Curricular de Medio Ambiente |
dc.contributor.orcid | Bohórquez Bedoya, Eliana [0000000153189570] |
dc.contributor.orcid | Lorke, Andreas [0000-0001-5533-1817] |
dc.contributor.orcid | Gómez Giraldo, Andrés [0000-0001-7103-9429] |
dc.contributor.cvlac | BOHÓRQUEZ BEDOYA, ELIANA |
dc.contributor.scopus | Bohórquez, Eliana [56957160300] |
dc.contributor.researchgate | https://www.researchgate.net/profile/Eliana-Bohorquez |
dc.contributor.researchgate | Bohórquez, Eliana [https://www.researchgate.net/profile/Eliana-Bohorquez] |
dc.contributor.googlescholar | Bohórquez, Eliana [Eliana Bohórquez] |
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