Analysis and diagnosis of the instability affecting "La Bonita" area, Amagá, Antioquia, Colombia

In the "La Bonita" sector (Amagá, Antioquia), between km 3+200 and km 3+500 of the Camilo C. Restrepo (Amagá) – El Cinco (Fredonia) road, which is above the rocks of the upper member of the Amagá formation (conformed mainly by interbedded claystones, sandstones and thin beds of coal), occu...

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Autores:
Álvarez Gutiérrez, Yennifer Yennifer
Montoya Cañola, Sandra Marcela
Rendón Giraldo, Diego Armando
Caballero Acosta, José Humberto
Tipo de recurso:
Article of journal
Fecha de publicación:
2015
Institución:
Universidad Nacional de Colombia
Repositorio:
Universidad Nacional de Colombia
Idioma:
spa
OAI Identifier:
oai:repositorio.unal.edu.co:unal/61863
Acceso en línea:
https://repositorio.unal.edu.co/handle/unal/61863
http://bdigital.unal.edu.co/60675/
Palabra clave:
55 Ciencias de la tierra / Earth sciences and geology
Amagá
Antioquia
Colombia
claystones
pressure to avoid expansion
expansive clays
morphodynamic processes
geotechnical characterization
X-ray diffraction
slope stability.
Rights
openAccess
License
Atribución-NoComercial 4.0 Internacional
Description
Summary:In the "La Bonita" sector (Amagá, Antioquia), between km 3+200 and km 3+500 of the Camilo C. Restrepo (Amagá) – El Cinco (Fredonia) road, which is above the rocks of the upper member of the Amagá formation (conformed mainly by interbedded claystones, sandstones and thin beds of coal), occur many instability processes that seriously affect the infrastructure of the area, and could be the result of the variations of mechanical and mineralogical properties of the claystones by effect of humidity fluctuations in the study area. According to the results obtained after multiple field trips, mapping of morphodynamic processes, subsoil explorations and laboratory tests, was determined that these materials, even as a rock, given their particular characteristics, have the ability to expand (changing their volume by about 10%) upon contact with water, generating expansion pressures up to 700kPa on the overlying materials, leading to the development of multiple slow morphodynamic processes (whose rate is related to winter seasons) that destabilize the ground.