Instability of Compacted Residual Soil

Static liquefaction of loose sands has been observed to initiate at stress ratios far less than the steady-state stress ratio. Different collapse surface concepts largely based on undrained triaxial test results have been proposed in the literature to explain the above instability phenomenon of loos...

Full description

Bibliographic Details
Main Authors: Sainulabdeen Mohamed Junaideen, Leslie George Tham, Chack Fan Lee
Format: Article
Language:English
Published: MDPI AG 2021-09-01
Series:Geosciences
Subjects:
Online Access:https://www.mdpi.com/2076-3263/11/10/403
_version_ 1797514468532420608
author Sainulabdeen Mohamed Junaideen
Leslie George Tham
Chack Fan Lee
author_facet Sainulabdeen Mohamed Junaideen
Leslie George Tham
Chack Fan Lee
author_sort Sainulabdeen Mohamed Junaideen
collection DOAJ
description Static liquefaction of loose sands has been observed to initiate at stress ratios far less than the steady-state stress ratio. Different collapse surface concepts largely based on undrained triaxial test results have been proposed in the literature to explain the above instability phenomenon of loose sands. Studies of the instability behavior of fill material derived from residual soils remain limited. The present study investigated the instability behavior of a compacted residual soil using the conventional undrained triaxial tests and specially equipped constant shear triaxial tests. The test results were characterized in the <i>p’: q: v</i> space using the current state parameter with respect to the steady-state line for the residual soil. A modified collapse surface that has gradients varying with <i>p’</i> and <i>v</i> was proposed for the loose residual soil to represent the instability states of undrained loading. Under constant shear stress conditions, the soil can mobilize stress ratios higher than those defined by the modified collapse surface. An instability surface was therefore presented for the instability states reached in static loading. Further, an alternative method of deducing the instability surface from the undrained stress paths was introduced.
first_indexed 2024-03-10T06:33:03Z
format Article
id doaj.art-bc393f3a87d54532a0b1f2e5307b6583
institution Directory Open Access Journal
issn 2076-3263
language English
last_indexed 2024-03-10T06:33:03Z
publishDate 2021-09-01
publisher MDPI AG
record_format Article
series Geosciences
spelling doaj.art-bc393f3a87d54532a0b1f2e5307b65832023-11-22T18:23:24ZengMDPI AGGeosciences2076-32632021-09-01111040310.3390/geosciences11100403Instability of Compacted Residual SoilSainulabdeen Mohamed Junaideen0Leslie George Tham1Chack Fan Lee2Department of Civil Engineering, South Eastern University of Sri Lanka, Oluvil 32360, Sri LankaDepartment of Civil Engineering, The University of Hong Kong, Pokfulam Road, Hong Kong, ChinaDepartment of Civil Engineering, The University of Hong Kong, Pokfulam Road, Hong Kong, ChinaStatic liquefaction of loose sands has been observed to initiate at stress ratios far less than the steady-state stress ratio. Different collapse surface concepts largely based on undrained triaxial test results have been proposed in the literature to explain the above instability phenomenon of loose sands. Studies of the instability behavior of fill material derived from residual soils remain limited. The present study investigated the instability behavior of a compacted residual soil using the conventional undrained triaxial tests and specially equipped constant shear triaxial tests. The test results were characterized in the <i>p’: q: v</i> space using the current state parameter with respect to the steady-state line for the residual soil. A modified collapse surface that has gradients varying with <i>p’</i> and <i>v</i> was proposed for the loose residual soil to represent the instability states of undrained loading. Under constant shear stress conditions, the soil can mobilize stress ratios higher than those defined by the modified collapse surface. An instability surface was therefore presented for the instability states reached in static loading. Further, an alternative method of deducing the instability surface from the undrained stress paths was introduced.https://www.mdpi.com/2076-3263/11/10/403instabilitystatic liquefactiontriaxial testconstant shearresidual soilcollapse surface
spellingShingle Sainulabdeen Mohamed Junaideen
Leslie George Tham
Chack Fan Lee
Instability of Compacted Residual Soil
Geosciences
instability
static liquefaction
triaxial test
constant shear
residual soil
collapse surface
title Instability of Compacted Residual Soil
title_full Instability of Compacted Residual Soil
title_fullStr Instability of Compacted Residual Soil
title_full_unstemmed Instability of Compacted Residual Soil
title_short Instability of Compacted Residual Soil
title_sort instability of compacted residual soil
topic instability
static liquefaction
triaxial test
constant shear
residual soil
collapse surface
url https://www.mdpi.com/2076-3263/11/10/403
work_keys_str_mv AT sainulabdeenmohamedjunaideen instabilityofcompactedresidualsoil
AT lesliegeorgetham instabilityofcompactedresidualsoil
AT chackfanlee instabilityofcompactedresidualsoil