FORECASTING SHALLOW LANDSLIDES USING PRECIPITATION DATA WITH THE HSB MODEL
The present study addresses a problem of slope stability by using a physically based model with the Hillslope- Storage Boussinesq (HSB) partial differential equation. This is used to evaluate shallow landslides, taking information from geotechnical parameters, slope profile, and rainfall. In this wo...
- Autores:
- Tipo de recurso:
- Fecha de publicación:
- 2017
- Institución:
- Universidad Industrial de Santander
- Repositorio:
- Repositorio UIS
- Idioma:
- spa
- OAI Identifier:
- oai:noesis.uis.edu.co:20.500.14071/5373
- Acceso en línea:
- https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/6384
https://noesis.uis.edu.co/handle/20.500.14071/5373
- Palabra clave:
- HSB equation
Landslides
Safety factor
Ecuación HSB
Deslizamientos
Factor de seguridad
- Rights
- openAccess
- License
- Attribution-NonCommercial 4.0 International (CC BY-NC 4.0)
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Attribution-NonCommercial 4.0 International (CC BY-NC 4.0)http://purl.org/coar/access_right/c_abf2info:eu-repo/semantics/openAccessAtribución-NoComercial-SinDerivadas 4.0 Internacional (CC BY-NC-ND 4.0)2017-06-142022-03-14T20:08:33Z2022-03-14T20:08:33Zhttps://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/638410.18273/revbol.v39n2-2017003https://noesis.uis.edu.co/handle/20.500.14071/5373The present study addresses a problem of slope stability by using a physically based model with the Hillslope- Storage Boussinesq (HSB) partial differential equation. This is used to evaluate shallow landslides, taking information from geotechnical parameters, slope profile, and rainfall. In this work, the equation was solved using finite difference methods in Python, by applying it to a theoretical area and calculating the safety factor. Five continuous periods of rainfall were considered in such equation. This data was taken from the records of the Automatic Weather Station in Manizales, Colombia. As a result, a monitoring of the stability slope through the safety factor was obtained, which was influenced in periods of 30 minutes, allowing a supervision of the surface soils landslide hazard by rainfall factor.Se aborda un problema de estabilidad de taludes, mediante la utilización de un modelo basado físicamente con la ecuación diferencial parcial HSB (Hillslope-Storage Boussinesq); utilizada para evaluar deslizamientos superficiales, tomando información de: parámetros geotécnicos, perfil de la ladera y precipitación. Esta ecuación, en este trabajo, se resolvió utilizando métodos de diferencias finitas en el ambiente del lenguaje de python. Se aplicó a una zona teórica y se calculó el factor de seguridad, considerando cinco periodos continuos de precipitación; estos datos fueron tomados de los registros de la estación del EMAS de la ciudad de Manizales. Como resultado se tiene un monitoreo a la estabilidad de la ladera a través del factor de seguridad, influenciado en periodos de 30 minutos, permitiendo realizar un monitoreo de la amenaza de deslizamientos de suelos superficiales por el factor de precipitación.application/pdftext/htmlspaUniversidad Industrial de Santanderhttps://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/6384/6611https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/6384/6950Boletín de Geología; Vol. 39 Núm. 2 (2017): Boletín de Geología; 49-56Boletín de Geología; Vol. 39 No. 2 (2017): Boletín de Geología; 49-56BOLETÍN DE GEOLOGÍA; v. 39 n. 2 (2017): Boletín de Geología; 49-562145-85530120-0283HSB equationLandslidesSafety factorEcuación HSBDeslizamientosFactor de seguridadFORECASTING SHALLOW LANDSLIDES USING PRECIPITATION DATA WITH THE HSB MODELDATOS DE PRECIPITACIÓN CON EL MODELO HSB PARA PRONÓSTICO DE DESLIZAMIENTO DE SUELOS SUPERFICIALESinfo:eu-repo/semantics/articlehttp://purl.org/coar/version/c_970fb48d4fbd8a85http://purl.org/coar/resource_type/c_2df8fbb1Peña-Rincón, Carlos Arturo20.500.14071/5373oai:noesis.uis.edu.co:20.500.14071/53732022-03-16 12:39:36.242metadata.onlyhttps://noesis.uis.edu.coDSpace at UISnoesis@uis.edu.co |
dc.title.en-US.fl_str_mv |
FORECASTING SHALLOW LANDSLIDES USING PRECIPITATION DATA WITH THE HSB MODEL |
dc.title.es-ES.fl_str_mv |
DATOS DE PRECIPITACIÓN CON EL MODELO HSB PARA PRONÓSTICO DE DESLIZAMIENTO DE SUELOS SUPERFICIALES |
title |
FORECASTING SHALLOW LANDSLIDES USING PRECIPITATION DATA WITH THE HSB MODEL |
spellingShingle |
FORECASTING SHALLOW LANDSLIDES USING PRECIPITATION DATA WITH THE HSB MODEL HSB equation Landslides Safety factor Ecuación HSB Deslizamientos Factor de seguridad |
title_short |
FORECASTING SHALLOW LANDSLIDES USING PRECIPITATION DATA WITH THE HSB MODEL |
title_full |
FORECASTING SHALLOW LANDSLIDES USING PRECIPITATION DATA WITH THE HSB MODEL |
title_fullStr |
FORECASTING SHALLOW LANDSLIDES USING PRECIPITATION DATA WITH THE HSB MODEL |
title_full_unstemmed |
FORECASTING SHALLOW LANDSLIDES USING PRECIPITATION DATA WITH THE HSB MODEL |
title_sort |
FORECASTING SHALLOW LANDSLIDES USING PRECIPITATION DATA WITH THE HSB MODEL |
dc.subject.en-US.fl_str_mv |
HSB equation Landslides Safety factor |
topic |
HSB equation Landslides Safety factor Ecuación HSB Deslizamientos Factor de seguridad |
dc.subject.es-ES.fl_str_mv |
Ecuación HSB Deslizamientos Factor de seguridad |
description |
The present study addresses a problem of slope stability by using a physically based model with the Hillslope- Storage Boussinesq (HSB) partial differential equation. This is used to evaluate shallow landslides, taking information from geotechnical parameters, slope profile, and rainfall. In this work, the equation was solved using finite difference methods in Python, by applying it to a theoretical area and calculating the safety factor. Five continuous periods of rainfall were considered in such equation. This data was taken from the records of the Automatic Weather Station in Manizales, Colombia. As a result, a monitoring of the stability slope through the safety factor was obtained, which was influenced in periods of 30 minutes, allowing a supervision of the surface soils landslide hazard by rainfall factor. |
publishDate |
2017 |
dc.date.accessioned.none.fl_str_mv |
2022-03-14T20:08:33Z |
dc.date.available.none.fl_str_mv |
2022-03-14T20:08:33Z |
dc.date.none.fl_str_mv |
2017-06-14 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article |
dc.type.coarversion.fl_str_mv |
http://purl.org/coar/version/c_970fb48d4fbd8a85 |
dc.type.coar.fl_str_mv |
http://purl.org/coar/resource_type/c_2df8fbb1 |
dc.identifier.none.fl_str_mv |
https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/6384 10.18273/revbol.v39n2-2017003 |
dc.identifier.uri.none.fl_str_mv |
https://noesis.uis.edu.co/handle/20.500.14071/5373 |
url |
https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/6384 https://noesis.uis.edu.co/handle/20.500.14071/5373 |
identifier_str_mv |
10.18273/revbol.v39n2-2017003 |
dc.language.none.fl_str_mv |
spa |
language |
spa |
dc.relation.none.fl_str_mv |
https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/6384/6611 https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/6384/6950 |
dc.rights.license.none.fl_str_mv |
Attribution-NonCommercial 4.0 International (CC BY-NC 4.0) |
dc.rights.coar.none.fl_str_mv |
http://purl.org/coar/access_right/c_abf2 |
dc.rights.accessrights.none.fl_str_mv |
info:eu-repo/semantics/openAccess |
dc.rights.creativecommons.none.fl_str_mv |
Atribución-NoComercial-SinDerivadas 4.0 Internacional (CC BY-NC-ND 4.0) |
rights_invalid_str_mv |
Attribution-NonCommercial 4.0 International (CC BY-NC 4.0) http://purl.org/coar/access_right/c_abf2 Atribución-NoComercial-SinDerivadas 4.0 Internacional (CC BY-NC-ND 4.0) |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf text/html |
dc.publisher.es-ES.fl_str_mv |
Universidad Industrial de Santander |
dc.source.es-ES.fl_str_mv |
Boletín de Geología; Vol. 39 Núm. 2 (2017): Boletín de Geología; 49-56 |
dc.source.en-US.fl_str_mv |
Boletín de Geología; Vol. 39 No. 2 (2017): Boletín de Geología; 49-56 |
dc.source.pt-BR.fl_str_mv |
BOLETÍN DE GEOLOGÍA; v. 39 n. 2 (2017): Boletín de Geología; 49-56 |
dc.source.none.fl_str_mv |
2145-8553 0120-0283 |
institution |
Universidad Industrial de Santander |
repository.name.fl_str_mv |
DSpace at UIS |
repository.mail.fl_str_mv |
noesis@uis.edu.co |
_version_ |
1814095193041797120 |