Análisis Lagrangiano de oleaje alrededor de arrecifes de coral

ilustraciones, diagramas

Autores:
Ramírez Monsalve, Juan Pablo
Tipo de recurso:
Fecha de publicación:
2023
Institución:
Universidad Nacional de Colombia
Repositorio:
Universidad Nacional de Colombia
Idioma:
spa
OAI Identifier:
oai:repositorio.unal.edu.co:unal/83869
Acceso en línea:
https://repositorio.unal.edu.co/handle/unal/83869
https://repositorio.unal.edu.co/
Palabra clave:
550 - Ciencias de la tierra
620 - Ingeniería y operaciones afines::627 - Ingeniería hidráulica
Ecología de arrecifes madrepóricos
Ecología de arrecifes
Coral reef ecology
Reef ecology
Corales
Vorticidad
Onda solitaria
Estructuras coherentes lagrangianas
Corals
Vorticity
Solitary wave
Lagrangian coherent structures
Rights
openAccess
License
Reconocimiento 4.0 Internacional
id UNACIONAL2_d3600bf0d7801dbc1f98363481111aaa
oai_identifier_str oai:repositorio.unal.edu.co:unal/83869
network_acronym_str UNACIONAL2
network_name_str Universidad Nacional de Colombia
repository_id_str
dc.title.spa.fl_str_mv Análisis Lagrangiano de oleaje alrededor de arrecifes de coral
dc.title.translated.eng.fl_str_mv Lagrangian analysis of wave dynamics around coral reefs
title Análisis Lagrangiano de oleaje alrededor de arrecifes de coral
spellingShingle Análisis Lagrangiano de oleaje alrededor de arrecifes de coral
550 - Ciencias de la tierra
620 - Ingeniería y operaciones afines::627 - Ingeniería hidráulica
Ecología de arrecifes madrepóricos
Ecología de arrecifes
Coral reef ecology
Reef ecology
Corales
Vorticidad
Onda solitaria
Estructuras coherentes lagrangianas
Corals
Vorticity
Solitary wave
Lagrangian coherent structures
title_short Análisis Lagrangiano de oleaje alrededor de arrecifes de coral
title_full Análisis Lagrangiano de oleaje alrededor de arrecifes de coral
title_fullStr Análisis Lagrangiano de oleaje alrededor de arrecifes de coral
title_full_unstemmed Análisis Lagrangiano de oleaje alrededor de arrecifes de coral
title_sort Análisis Lagrangiano de oleaje alrededor de arrecifes de coral
dc.creator.fl_str_mv Ramírez Monsalve, Juan Pablo
dc.contributor.advisor.none.fl_str_mv Osorio Arias, Andrés Fernando
Hernandez-Carrasco, Ismael
dc.contributor.author.none.fl_str_mv Ramírez Monsalve, Juan Pablo
dc.contributor.researchgroup.spa.fl_str_mv Oceanicos Grupo de Oceanografía E Ingeniería Costera de la Universidad Nacional
dc.contributor.orcid.spa.fl_str_mv Hernández Carrasco, Ismael [0000-0002-4574-0198]
dc.subject.ddc.spa.fl_str_mv 550 - Ciencias de la tierra
620 - Ingeniería y operaciones afines::627 - Ingeniería hidráulica
topic 550 - Ciencias de la tierra
620 - Ingeniería y operaciones afines::627 - Ingeniería hidráulica
Ecología de arrecifes madrepóricos
Ecología de arrecifes
Coral reef ecology
Reef ecology
Corales
Vorticidad
Onda solitaria
Estructuras coherentes lagrangianas
Corals
Vorticity
Solitary wave
Lagrangian coherent structures
dc.subject.lemb.spa.fl_str_mv Ecología de arrecifes madrepóricos
Ecología de arrecifes
dc.subject.lemb.eng.fl_str_mv Coral reef ecology
Reef ecology
dc.subject.proposal.spa.fl_str_mv Corales
Vorticidad
Onda solitaria
Estructuras coherentes lagrangianas
dc.subject.proposal.eng.fl_str_mv Corals
Vorticity
Solitary wave
Lagrangian coherent structures
description ilustraciones, diagramas
publishDate 2023
dc.date.accessioned.none.fl_str_mv 2023-05-25T16:39:58Z
dc.date.available.none.fl_str_mv 2023-05-25T16:39:58Z
dc.date.issued.none.fl_str_mv 2023-05-24
dc.type.spa.fl_str_mv Trabajo de grado - Maestría
dc.type.driver.spa.fl_str_mv info:eu-repo/semantics/masterThesis
dc.type.version.spa.fl_str_mv info:eu-repo/semantics/acceptedVersion
dc.type.content.spa.fl_str_mv Text
dc.type.redcol.spa.fl_str_mv http://purl.org/redcol/resource_type/TM
status_str acceptedVersion
dc.identifier.uri.none.fl_str_mv https://repositorio.unal.edu.co/handle/unal/83869
dc.identifier.instname.spa.fl_str_mv Universidad Nacional de Colombia
dc.identifier.reponame.spa.fl_str_mv Repositorio Institucional Universidad Nacional de Colombia
dc.identifier.repourl.spa.fl_str_mv https://repositorio.unal.edu.co/
url https://repositorio.unal.edu.co/handle/unal/83869
https://repositorio.unal.edu.co/
identifier_str_mv Universidad Nacional de Colombia
Repositorio Institucional Universidad Nacional de Colombia
dc.language.iso.spa.fl_str_mv spa
language spa
dc.relation.indexed.spa.fl_str_mv RedCol
LaReferencia
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dc.rights.license.spa.fl_str_mv Reconocimiento 4.0 Internacional
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dc.publisher.spa.fl_str_mv Universidad Nacional de Colombia
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dc.publisher.faculty.spa.fl_str_mv Facultad de Minas
dc.publisher.place.spa.fl_str_mv Medellín, Colombia
dc.publisher.branch.spa.fl_str_mv Universidad Nacional de Colombia - Sede Medellín
institution Universidad Nacional de Colombia
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spelling Reconocimiento 4.0 Internacionalhttp://creativecommons.org/licenses/by/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Osorio Arias, Andrés Fernando7f3dd14c4e66765c34f0d73a9c0b17faHernandez-Carrasco, Ismaelf792412fa801f7c43b967519b17bcbb1600Ramírez Monsalve, Juan Pablo572885255b36aa4868b193d117cb064aOceanicos Grupo de Oceanografía E Ingeniería Costera de la Universidad NacionalHernández Carrasco, Ismael [0000-0002-4574-0198]2023-05-25T16:39:58Z2023-05-25T16:39:58Z2023-05-24https://repositorio.unal.edu.co/handle/unal/83869Universidad Nacional de ColombiaRepositorio Institucional Universidad Nacional de Colombiahttps://repositorio.unal.edu.co/ilustraciones, diagramasDebido a su inherente naturaleza turbulenta, la dinámica de los océanos es muy compleja. Podemos modelar los principales patrones de transporte de la circulación oceánica en meso- y submeso-escalas, O (0,1-100 km, horas-meses) utilizando enfoques de sistemas dinámicos, pero la riqueza extrema en microescalas O (0,001-10 m, segundos) y sus patrones de circulación, hace que la evaluación de los fenómenos de transporte oceánico sea una tarea extraordinariamente complicada. En la microescala podemos encontrar ecosistemas de arrecifes coralinos, que en los últimos años han cobrado notoria importancia por los efectos que pueden generar sobre la hidrodinámica del flujo incidente, en áreas que van desde la biología hasta la ingeniería debido a su papel como estructuras de protección costera. A pesar de los estudios realizados para comprender la hidrodinámica en torno a estos ecosistemas, aún no existe una idea clara de cómo los diferentes tipos de geometría de las colonias de coral condicionan los patrones de transporte que se desarrollan en el flujo. Uno de los tipos de técnicas que más contribuye a la comprensión de los patrones de transporte y a la descripción de la topología del flujo es la conocida con el nombre de Estructuras Coherentes Lagrangianas (LCS por sus siglas en inglés), que es una generalización de las variedades inestables y estables de puntos hiperbólicos en sistemas dependientes del tiempo. En esta tesis evaluamos la viabilidad de utilizar el concepto LCS para describir las propiedades de transporte y mezcla en flujos altamente fluctuantes a microescala alrededor de geometrías de coral. En particular, estudiamos los patrones de transporte inducidos por la interacción entre una ola solitaria y objetos sumergidos de diferente geometría, que se aproximan a la geometría presente en los corales. Usamos datos de velocidad de las salidas del modelo RANS-VOF. Los escenarios analizados consisten en la variación del número de Reynolds, la relación entre la altura de la ola, H, y la profundidad del agua, h, con la altura del coral, L (H/L y h/L , respectivamente) y la forma de éste. Los patrones de transporte se estudian mediante el cálculo de estructuras coherentes lagrangianas con la implementación del método del exponente de Lyapunov de tiempo finito (FTLE por sus siglas en inglés), y se comparan con el campo de vorticidad y el campo de criterio Q (Okubo-Weiss). Encontramos que el campo de vorticidad tiene una mejor correlación con el campo FTLE (geometría LCS) que con el campo Q, lo que sugiere que la topología de flujo está más controlada por el proceso de vorticidad obtenido por un flujo cortante que por los mismos vórtices(regiones de rotación pura). Para los corales representados por geometrías rectangulares, las LCS tienen forma de espiral, se forman sobre y en la parte posterior del coral. Ambas LCS permanecen adheridas al objeto sumergido una vez que h/L y H/L comienzan a disminuir. Para los corales con geometrías triangulares, la geometría de las LCS se caracteriza por una doble espiral que permanece unida a la cresta del coral. La doble espiral es generada por un anillo vorticial(vortex ring) que aparece cuando la ola pasa sobre el coral. Cuando la altura del coral comienza a ser comparable con la profundidad del agua, los patrones LCS descritos anteriormente comienzan a deformarse debido a la falta de profundidad del agua para evolucionar, por lo tanto, para las geometrías triangulares y rectangulares, tenemos un proceso de ruptura de olas, donde parece que el LCS actúa como un "falso fondo'' generando inestabilidades en la ola incidente que inducen la ruptura de la misma. Las LCS más cercanas a la superficie libre también parecen controlar la curvatura de la misma después de que se produzcan las roturas. Las LCS para el coral triangular presentan valores mayores del campo FTLE que el rectangular, lo que sugiere que los corales que tienen una forma aproximadamente triangular aumentan la mezcla del flujo con un gran impacto en la dispersión del material transportado (es decir, nutrientes, oxígeno, etc.), respecto a las geometrías rectangulares. (Texto tomado de la fuente)Owing to its inherent turbulent nature, ocean dynamics is highly complex. We can model the main transport patterns of the ocean circulation at meso- and submeso-scales, O(0.1-100 km, hours-months) using dynamical systems approaches, but the extreme richness at microscales O(0.001-10m, seconds) circulation patterns, makes the assessment of water pathways and the study of oceanic transport phenomena an extraordinarily complicated task. At microscales we can find coral reef ecosystems, which in recent years have gained notorious importance regarding the effects they can generate on the hydrodynamics of the incident flow, in areas from biology to engineering due to their role as structures of coastal protection. Despite the studies carried out to understand the hydrodynamics around these ecosystems, there is still not a clear idea of how the different types of geometry of the coral colonies condition the transport patterns that develop in the flow. One type of techniques contributing most to the understanding of transport patterns and the description of flow’s topology is the one known under the name of Lagrangian Coherent Structures, which is a generalization of the unstable and stable manifolds of hyperbolic points in time independent systems to finite-time and time-dependent systems. In this thesis we evaluate the feasibility of using the LCS concept to describe the transport and mixing properties in highly fluctuating flows at microscales around coral geometries. In particular, we study the transport patterns induced by the interaction between a solitary wave with submerged objects of different geometry, that approximate the geometry present in corals. We use velocity data from RANS-VOF model outputs. The analized scenarios consist in variation of Reynolds number, the ratio between the wave height, H, and the water depth, h, with the coral heigth, L (H/L and h/L, respectively) and shape. The transport patterns are studied through the computation of Lagrangian coherent structures with the implementation of the finite-time Lyapunov exponent (FTLE) method, and compared with the vorticity field and the Q criterion field. We found that vorticity field has a better correlation with the FTLE field (LCS geometry) than the Q field, suggesting that the flow topology is controled more for vorticity process obtained by a shear flow than for vortices itself (pure rotation regions). For corals represented by rectangular geometries, the LCS have an spiral form, and are formed above and at the lee side of the coral. Both LCS remain attached to the submerged object once h/L and H/L starts to decrease. For the corals with triangular geometries, the LCS geometry is characterized by a double spiral that remains attached to coral’s crest. The double spiral is generated by a vortex ring that appears when the wave pass over the coral. When coral’s height starts to be comparable to the water depth, the LCS patterns described above, start to be deformed due to the lack of water depth to evolve, so for both triangular and rectangular geometries, we have a wave breaking process, where it seems that the LCS acts like a “fake bottom” generating instabilities in the incident wave that induce the break of it. The closest LCS ridges to the free surface also appears to control the curvature of it after the breaks takes place. The LCS for the triangular coral presents larger values of the FTLE field than the rectangular one, suggesting that corals that have an approximately triangular shape increase the flow mixing processes with a large impact on the spreading of the transported material (i.e nutrients, oxygen, etc), with respect to the rectangular ones.MaestríaMagíster en Ingeniería - Recursos HidráulicosSe usa la metodología de los FTLE para obtener los campos de las estructuras coherentes lagrangianas (LCS) para el estudio de patrones de mezcla,transporte y rotura del oleaje al interacturar con un obstáculo sumergido (coral)Interacción flujo estructura en ecosistemas marinosÁrea Curricular de Medio Ambientexiii, 69 páginasapplication/pdfspaUniversidad Nacional de ColombiaMedellín - Minas - Maestría en Ingeniería - Recursos HidráulicosFacultad de MinasMedellín, ColombiaUniversidad Nacional de Colombia - Sede Medellín550 - Ciencias de la tierra620 - Ingeniería y operaciones afines::627 - Ingeniería hidráulicaEcología de arrecifes madrepóricosEcología de arrecifesCoral reef ecologyReef ecologyCoralesVorticidadOnda solitariaEstructuras coherentes lagrangianasCoralsVorticitySolitary waveLagrangian coherent structuresAnálisis Lagrangiano de oleaje alrededor de arrecifes de coralLagrangian analysis of wave dynamics around coral reefsTrabajo de grado - Maestríainfo:eu-repo/semantics/masterThesisinfo:eu-repo/semantics/acceptedVersionTexthttp://purl.org/redcol/resource_type/TMRedColLaReferenciaAndersson, A. 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Cost and time-effective method for multi-scale measures of rugosity, fractal dimension, and vector dispersion from coral reef 3d models.EstudiantesInvestigadoresLICENSElicense.txtlicense.txttext/plain; charset=utf-85879https://repositorio.unal.edu.co/bitstream/unal/83869/3/license.txteb34b1cf90b7e1103fc9dfd26be24b4aMD53ORIGINAL1036670881.2023.pdf1036670881.2023.pdfTesis de Maestría en Ingeniería - Recursos Hidráulicosapplication/pdf13046552https://repositorio.unal.edu.co/bitstream/unal/83869/4/1036670881.2023.pdff467d22abcfbcb5430bdedc3c18c2de5MD54THUMBNAIL1036670881.2023.pdf.jpg1036670881.2023.pdf.jpgGenerated Thumbnailimage/jpeg4192https://repositorio.unal.edu.co/bitstream/unal/83869/5/1036670881.2023.pdf.jpgd6658f80e12960134cd98b50270e11d3MD55unal/83869oai:repositorio.unal.edu.co:unal/838692023-08-06 23:03:46.908Repositorio Institucional Universidad Nacional de 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