dc.contributor | Ávila Álvarez, Guillermo Eduardo | |
dc.creator | Moncayo Legarda, Carlos Steven | |
dc.date.accessioned | 2022-02-01T13:43:49Z | |
dc.date.available | 2022-02-01T13:43:49Z | |
dc.date.created | 2022-02-01T13:43:49Z | |
dc.date.issued | 2021 | |
dc.identifier | https://repositorio.unal.edu.co/handle/unal/80825 | |
dc.identifier | Universidad Nacional de Colombia | |
dc.identifier | Repositorio Institucional Universidad Nacional de Colombia | |
dc.identifier | https://repositorio.unal.edu.co/ | |
dc.description.abstract | El análisis de los deslizamientos y los daños derivados de estos procesos han requerido el esfuerzo de los profesionales e investigadores en el área de la geotecnia a través de la implementación de herramientas como los estudios de amenaza, vulnerabilidad y riesgo. Uno de los temas que ha recibido especial atención en los últimos años es la evaluación de la distancia de viaje, a través de modelos simples o modelos más sofisticados que involucran análisis más detallados, esto con el fin de mejorar la evaluación de la amenaza. En este estudio, se obtuvo un conjunto de datos con parámetros característicos de 199 deslizamientos en la región Andina de Colombia a partir del inventario digital del Sistema de Información de Movimientos en Masa (SIMMA) implementado por el Servicio Geológico Colombiano. Los análisis muestran que los movimientos en masa de la región se desarrollan en una gran variedad de materiales y son desencadenados principalmente por la acción de la lluvia, además exhiben en su mayoría una movilidad limitada y una magnitud relativamente pequeña. Por otra parte, se evaluó el efecto de distintos factores de influencia en el alcance de los deslizamientos, obteniendo así modelos empíricos para su predicción mediante técnicas de regresión simple y múltiple. Los resultados revelan que el volumen de la masa desplazada, el ángulo del talud antes de la falla, la altura vertical máxima y el ambiente geomorfológico son los factores predominantes en los modelos para la evaluación de la distancia de viaje de los movimientos en masa de la región, asimismo, se encontró una buena correlación entre el área planimétrica y el volumen del evento. Los modelos propuestos muestran un ajuste razonable entre los valores observados y predichos, y para el caso colombiano muestran una capacidad de predicción superior al resto de modelos disponibles aplicados a los datos de este estudio. Las ecuaciones de predicción fueron posteriormente usadas para elaborar un mapa de distancias de viaje que delimita zonas de amenaza para distintas probabilidades de excedencia. Los modelos empíricos presentados en este trabajo son aplicables para la región Andina y otras regiones con similar configuración geológica y geomorfológica y constituyen un aporte para los procesos de gestión de riesgo por movimientos en masa en el país. (Texto tomado de la fuente). | |
dc.description.abstract | The analysis of the landslides and the damages derived from these processes have required the effort of professionals and researchers in the area of geotechnics through the implementation of tools such as hazard, vulnerability and risk assessment. One of the topics that has received special attention in recent years is the evaluation of travel distance, through simple models or more sophisticated models that involve more detailed analysis, in order to improve hazard assessment. In this study, a dataset with characteristic parameters of 199 landslides in the Andean region of Colombia was obtained from the digital inventory of the Mass Movement Information System (SIMMA) implemented by the Colombian Geological Survey. The analysis shows that mass movements in the region are developed in a wide variety of materials and are mainly triggered by the action of rainfall. In addition, they mostly exhibit limited mobility and relatively small magnitude. On the other hand, the effect of different influential factors on the reach of the landslides was evaluated, thus obtaining empirical models for their prediction by means of simple and multiple regression techniques. The results reveal that the volume of the displaced mass, the angle of the slope before the failure, the maximum vertical height and the geomorphological environment are the predominant factors in the models for the evaluation of the travel distance of the mass movements in the region, likewise, a good correlation was found between the planimetric area and the volume of the event. The proposed models show a reasonable fit between the observed and predicted values, and for the Colombian case they show a higher prediction capacity than the rest of the available models applied to the data of this study. The prediction equations were subsequently used to develop a travel distance map that delineates hazard zones for different exceedance probabilities. The empirical models presented in this work are applicable to the Andean region and other regions with similar geological and geomorphological settings and constitute a contribution to the risk management processes for mass movements in the country. | |
dc.language | spa | |
dc.publisher | Universidad Nacional de Colombia | |
dc.publisher | Bogotá - Ingeniería - Maestría en Ingeniería - Geotecnia | |
dc.publisher | Departamento de Ingeniería Civil y Agrícola | |
dc.publisher | Facultad de Ingeniería | |
dc.publisher | Bogotá, Colombia | |
dc.publisher | Universidad Nacional de Colombia - Sede Bogotá | |
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dc.rights | Atribución-SinDerivadas 4.0 Internacional | |
dc.rights | http://creativecommons.org/licenses/by-nd/4.0/ | |
dc.rights | info:eu-repo/semantics/openAccess | |
dc.title | Evaluación de la distancia de viaje de movimientos en masa en Colombia a partir de registros históricos | |
dc.type | Trabajo de grado - Maestría | |