Mapping of slope instability in steeply sloping basins using the infinite slope approach.

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Areas with a steep slope and with the presence of rain are susceptible to landslides, which in turn can cause other disasters. The objective of this research is to determine the landslide hazard map using deterministic methods, as a case study in the Cuyocuyo river basin, located in the northeast ar...

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Detalles Bibliográficos
Autores: Alfaro Alejo, Roberto, Mamani Gomez, Jose A., Pilares Hualpa, Isidro A.
Formato: artículo
Fecha de Publicación:2022
Institución:Universidad Privada de Tacna
Repositorio:Revistas - Universidad Privada de Tacna
Lenguaje:español
OAI Identifier:oai:revistas.upt.edu.pe:article/601
Enlace del recurso:https://revistas.upt.edu.pe/ojs/index.php/vestsc/article/view/601
Nivel de acceso:acceso abierto
Materia:Inestabilidad
Cuyocuyo
talud infinito
sistema de información geográfica
deslizamiento
Instability
infinite slope
Geographic Information System
landslide
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spelling Mapping of slope instability in steeply sloping basins using the infinite slope approach.Mapeo de inestabilidad de laderas en cuencas de fuerte pendiente mediante el enfoque de talud infinito.Alfaro Alejo, RobertoMamani Gomez, Jose A.Pilares Hualpa, Isidro A.InestabilidadCuyocuyotalud infinitosistema de información geográficadeslizamientoInstabilityCuyocuyoinfinite slopeGeographic Information SystemlandslideAreas with a steep slope and with the presence of rain are susceptible to landslides, which in turn can cause other disasters. The objective of this research is to determine the landslide hazard map using deterministic methods, as a case study in the Cuyocuyo river basin, located in the northeast area of the department of Puno, belonging to the Amazon watershed, considered a moderately rainy and steep slopes. The mapping of ground instability is carried out considering landslides as surface translational, controlled by convergence of groundwater flow, using the infinite slope model. The data required to implement the model includes topography, soil properties, and water states that are highly variable in both space and time. The landslide inventory is used as verification at the points of occurrence. As results, for the saturated, semi-saturated and dry soil conditions, the safety factor is between the unstable and very unstable classes, at 42%, 38% and 18% of the basin area, respectively; which is indicative of a landslide-prone area. The information provided by landslide susceptibility maps helps authorities and technicians to adopt hazard reduction strategies for existing and future landslides through prevention, mitigation and evasion.Las zonas de fuerte pendiente y con presencia de lluvias son susceptibles a deslizamientos que a su vez pueden provocar otros desastres. El objetivo de esta investigación es determinar el mapa de peligro por deslizamiento mediante métodos determinísticos, como un estudio de caso en la cuenca del río Cuyocuyo, ubicado en la zona nororiental del departamento de Puno, perteneciente a la vertiente amazónica, considerada como zona moderadamente lluviosa y de pendientes abruptas. El mapeo de la inestabilidad del terreno, se realiza considerando los deslizamientos como traslacional superficial, controlado por convergencia del flujo subterráneo, utilizando el modelo de talud infinito. Los datos requeridos para implementar el modelo incluyen topografía, propiedades del suelo y estados hídricos que son altamente variables tanto en el espacio y el tiempo. El inventario de deslizamientos es utilizado como verificación en los puntos de ocurrencia. Como resultados se ha obtenido para las condiciones de suelo saturado, semisaturado y seco el factor de seguridad está entre las clases inestable a muy inestable, en un 42%, 38% y 18% del área de la cuenca respectivamente; lo que es un indicativo de zona propensa a deslizamientos. La información dada por los mapas de susceptibilidad a deslizamiento, ayuda a las autoridades y técnicos para que adopten estrategias de reducción de peligro por deslizamientos existentes y futuros por medio de la prevención, mitigación y evasión.Universidad Privada de Tacna2022-05-24info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdftext/htmlhttps://revistas.upt.edu.pe/ojs/index.php/vestsc/article/view/60110.47796/ves.v11i1.601REVISTA VERITAS ET SCIENTIA - UPT; Vol. 11 No. 1 (2022): Veritas et Scientia; 112 - 124REVISTA VERITAS ET SCIENTIA - UPT; Vol. 11 Núm. 1 (2022): Veritas et Scientia; 112 - 1242617-06392307-513910.47796/ves.v11i1reponame:Revistas - Universidad Privada de Tacnainstname:Universidad Privada de Tacnainstacron:UPTspahttps://revistas.upt.edu.pe/ojs/index.php/vestsc/article/view/601/568https://revistas.upt.edu.pe/ojs/index.php/vestsc/article/view/601/584Derechos de autor 2022 Roberto Alfaro Alejo, Jose A. Mamani Gomez, Isidro A. Pilares Hualpainfo:eu-repo/semantics/openAccessoai:revistas.upt.edu.pe:article/6012024-10-26T19:31:18Z
dc.title.none.fl_str_mv Mapping of slope instability in steeply sloping basins using the infinite slope approach.
Mapeo de inestabilidad de laderas en cuencas de fuerte pendiente mediante el enfoque de talud infinito.
title Mapping of slope instability in steeply sloping basins using the infinite slope approach.
spellingShingle Mapping of slope instability in steeply sloping basins using the infinite slope approach.
Alfaro Alejo, Roberto
Inestabilidad
Cuyocuyo
talud infinito
sistema de información geográfica
deslizamiento
Instability
Cuyocuyo
infinite slope
Geographic Information System
landslide
title_short Mapping of slope instability in steeply sloping basins using the infinite slope approach.
title_full Mapping of slope instability in steeply sloping basins using the infinite slope approach.
title_fullStr Mapping of slope instability in steeply sloping basins using the infinite slope approach.
title_full_unstemmed Mapping of slope instability in steeply sloping basins using the infinite slope approach.
title_sort Mapping of slope instability in steeply sloping basins using the infinite slope approach.
dc.creator.none.fl_str_mv Alfaro Alejo, Roberto
Mamani Gomez, Jose A.
Pilares Hualpa, Isidro A.
author Alfaro Alejo, Roberto
author_facet Alfaro Alejo, Roberto
Mamani Gomez, Jose A.
Pilares Hualpa, Isidro A.
author_role author
author2 Mamani Gomez, Jose A.
Pilares Hualpa, Isidro A.
author2_role author
author
dc.subject.none.fl_str_mv Inestabilidad
Cuyocuyo
talud infinito
sistema de información geográfica
deslizamiento
Instability
Cuyocuyo
infinite slope
Geographic Information System
landslide
topic Inestabilidad
Cuyocuyo
talud infinito
sistema de información geográfica
deslizamiento
Instability
Cuyocuyo
infinite slope
Geographic Information System
landslide
description Areas with a steep slope and with the presence of rain are susceptible to landslides, which in turn can cause other disasters. The objective of this research is to determine the landslide hazard map using deterministic methods, as a case study in the Cuyocuyo river basin, located in the northeast area of the department of Puno, belonging to the Amazon watershed, considered a moderately rainy and steep slopes. The mapping of ground instability is carried out considering landslides as surface translational, controlled by convergence of groundwater flow, using the infinite slope model. The data required to implement the model includes topography, soil properties, and water states that are highly variable in both space and time. The landslide inventory is used as verification at the points of occurrence. As results, for the saturated, semi-saturated and dry soil conditions, the safety factor is between the unstable and very unstable classes, at 42%, 38% and 18% of the basin area, respectively; which is indicative of a landslide-prone area. The information provided by landslide susceptibility maps helps authorities and technicians to adopt hazard reduction strategies for existing and future landslides through prevention, mitigation and evasion.
publishDate 2022
dc.date.none.fl_str_mv 2022-05-24
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv https://revistas.upt.edu.pe/ojs/index.php/vestsc/article/view/601
10.47796/ves.v11i1.601
url https://revistas.upt.edu.pe/ojs/index.php/vestsc/article/view/601
identifier_str_mv 10.47796/ves.v11i1.601
dc.language.none.fl_str_mv spa
language spa
dc.relation.none.fl_str_mv https://revistas.upt.edu.pe/ojs/index.php/vestsc/article/view/601/568
https://revistas.upt.edu.pe/ojs/index.php/vestsc/article/view/601/584
dc.rights.none.fl_str_mv Derechos de autor 2022 Roberto Alfaro Alejo, Jose A. Mamani Gomez, Isidro A. Pilares Hualpa
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Derechos de autor 2022 Roberto Alfaro Alejo, Jose A. Mamani Gomez, Isidro A. Pilares Hualpa
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
text/html
dc.publisher.none.fl_str_mv Universidad Privada de Tacna
publisher.none.fl_str_mv Universidad Privada de Tacna
dc.source.none.fl_str_mv REVISTA VERITAS ET SCIENTIA - UPT; Vol. 11 No. 1 (2022): Veritas et Scientia; 112 - 124
REVISTA VERITAS ET SCIENTIA - UPT; Vol. 11 Núm. 1 (2022): Veritas et Scientia; 112 - 124
2617-0639
2307-5139
10.47796/ves.v11i1
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instname_str Universidad Privada de Tacna
instacron_str UPT
institution UPT
reponame_str Revistas - Universidad Privada de Tacna
collection Revistas - Universidad Privada de Tacna
repository.name.fl_str_mv
repository.mail.fl_str_mv
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