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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Main Authors: Deepak R. Bhat, Janusz V. Kozubal, Matylda Tankiewicz
Format: Article
Language:English
Published: MDPI AG 2021-04-01
Series:Materials
Subjects:
Online Access:https://www.mdpi.com/1996-1944/14/8/1968
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spelling 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
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