Extended Residual-State Creep Test and Its Application for Landslide Stability Assessment
This paper contains the results of a newly developed residual-state creep test performed to determine the behavior of a selected geomaterial in the context of reactivated landslides. Soil and rock creep is a time-dependent phenomenon in which a deformation occurs under constant stress. Based on the...
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doaj-f3db70fe8d9b45b2aa25c3181331d9292021-04-14T23:04:31ZengMDPI AGMaterials1996-19442021-04-01141968196810.3390/ma14081968Extended Residual-State Creep Test and Its Application for Landslide Stability AssessmentDeepak R. Bhat0Janusz V. Kozubal1Matylda Tankiewicz2Engineering Division, Okuyama Boring Co. Ltd., Tokyo 103-0004, JapanFaculty of Civil Engineering, Wrocław University of Science and Technology, 50-370 Wrocław, PolandDepartment of Building Engineering, Wrocław University of Environmental and Life Sciences, 50-375 Wrocław, PolandThis paper contains the results of a newly developed residual-state creep test performed to determine the behavior of a selected geomaterial in the context of reactivated landslides. Soil and rock creep is a time-dependent phenomenon in which a deformation occurs under constant stress. Based on the examination results, it was found that the tested clayey material (from Kobe, Japan) shows tertiary creep behavior only under shear stress higher than the residual strength condition and primary and secondary creep behavior under shear stress lower or equal to the residual strength condition. Based on the data, a model for predicting the critical or failure time is introduced. The study traces the development of the limit state based on the contact model corresponding to Blair’s body. The time to occurrence of the conditions necessary for unlimited creep on the surface is estimated. As long-term precipitation and infiltrating water in the area of the landslides are identified as the key phenomena initiating collapse, the work focuses on the prediction of landslides with identified surfaces of potential damage as a result of changes in the saturation state. The procedure outlined is applied to a case study and considerations as to when the necessary safety work should be carried out are presented.https://www.mdpi.com/1996-1944/14/8/1968residual-state creepsaturation frontlandslides |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Deepak R. Bhat Janusz V. Kozubal Matylda Tankiewicz |
spellingShingle |
Deepak R. Bhat Janusz V. Kozubal Matylda Tankiewicz Extended Residual-State Creep Test and Its Application for Landslide Stability Assessment Materials residual-state creep saturation front landslides |
author_facet |
Deepak R. Bhat Janusz V. Kozubal Matylda Tankiewicz |
author_sort |
Deepak R. Bhat |
title |
Extended Residual-State Creep Test and Its Application for Landslide Stability Assessment |
title_short |
Extended Residual-State Creep Test and Its Application for Landslide Stability Assessment |
title_full |
Extended Residual-State Creep Test and Its Application for Landslide Stability Assessment |
title_fullStr |
Extended Residual-State Creep Test and Its Application for Landslide Stability Assessment |
title_full_unstemmed |
Extended Residual-State Creep Test and Its Application for Landslide Stability Assessment |
title_sort |
extended residual-state creep test and its application for landslide stability assessment |
publisher |
MDPI AG |
series |
Materials |
issn |
1996-1944 |
publishDate |
2021-04-01 |
description |
This paper contains the results of a newly developed residual-state creep test performed to determine the behavior of a selected geomaterial in the context of reactivated landslides. Soil and rock creep is a time-dependent phenomenon in which a deformation occurs under constant stress. Based on the examination results, it was found that the tested clayey material (from Kobe, Japan) shows tertiary creep behavior only under shear stress higher than the residual strength condition and primary and secondary creep behavior under shear stress lower or equal to the residual strength condition. Based on the data, a model for predicting the critical or failure time is introduced. The study traces the development of the limit state based on the contact model corresponding to Blair’s body. The time to occurrence of the conditions necessary for unlimited creep on the surface is estimated. As long-term precipitation and infiltrating water in the area of the landslides are identified as the key phenomena initiating collapse, the work focuses on the prediction of landslides with identified surfaces of potential damage as a result of changes in the saturation state. The procedure outlined is applied to a case study and considerations as to when the necessary safety work should be carried out are presented. |
topic |
residual-state creep saturation front landslides |
url |
https://www.mdpi.com/1996-1944/14/8/1968 |
work_keys_str_mv |
AT deepakrbhat extendedresidualstatecreeptestanditsapplicationforlandslidestabilityassessment AT januszvkozubal extendedresidualstatecreeptestanditsapplicationforlandslidestabilityassessment AT matyldatankiewicz extendedresidualstatecreeptestanditsapplicationforlandslidestabilityassessment |
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