Methodology for mudflow hazard assessment triggered by rainfall, in El Rollo Watershed, San Bernardo, Nariño

Torrential rainfalls are considered destructive processes that take place around the world, these are generated in mountainous areas and are deposited in alluvial fans or plains commonly occupied by human settlements, hence transporting a large volume of sediment, this case particularly applies for...

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Autores:
Tipo de recurso:
http://purl.org/coar/resource_type/c_6718
Fecha de publicación:
2022
Institución:
Universidad Pedagógica y Tecnológica de Colombia
Repositorio:
RiUPTC: Repositorio Institucional UPTC
Idioma:
spa
OAI Identifier:
oai:repositorio.uptc.edu.co:001/12345
Acceso en línea:
https://revistas.uptc.edu.co/index.php/ingenieria_sogamoso/article/view/14268
https://repositorio.uptc.edu.co/handle/001/12345
Palabra clave:
sludge flow
threat
liquid flow
sediment volume
geographic information systems
flujo de lodos
amenaza
caudal líquido
volumen de sedimentos
sistemas de información geográfica
Rights
License
http://purl.org/coar/access_right/c_abf219
Description
Summary:Torrential rainfalls are considered destructive processes that take place around the world, these are generated in mountainous areas and are deposited in alluvial fans or plains commonly occupied by human settlements, hence transporting a large volume of sediment, this case particularly applies for “El Rollo” creek micro-basin, its water network flows throughout theurban area of “San Bernardo” village, therefore, it shows a potential for the occurrence of this kind of event. In this work, a methodology was conducted by the implementation of Geographic Information Systems was carried out for the evaluation of the threat due to the flow of sludge formed under rain events. The implementation of a mathematical FLO-2D model allowed a rainfall to flow transition used to determinate the hydric characteristics on the area, subsequently, the threat level in the basin is evaluated through the modeling of a torrential event proposed for different scenarios, establishing depths and peak flow speed rates for each setting over potential deposition zones. Once the simulation results were obtained a hazard map was developed based on the event intensity and its frequency of occurrence.