Effect of hysteresis on the stability of residual soil slope

Soil-water characteristic curve (SWCC) is an essential parameter in unsaturated soil mechanics. Matric suction in unsaturated residual soils changes with varying climatic conditions associated with cyclic drying-wetting conditions that result in hysteresis in the SWCC. The soil mechanical behaviour...

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Main Authors: Christofer Kristo, Harianto Rahardjo, Alfrendo Satyanaga
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2019-09-01
Series:International Soil and Water Conservation Research
Online Access:http://www.sciencedirect.com/science/article/pii/S2095633918300789
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author Christofer Kristo
Harianto Rahardjo
Alfrendo Satyanaga
author_facet Christofer Kristo
Harianto Rahardjo
Alfrendo Satyanaga
author_sort Christofer Kristo
collection DOAJ
description Soil-water characteristic curve (SWCC) is an essential parameter in unsaturated soil mechanics. Matric suction in unsaturated residual soils changes with varying climatic conditions associated with cyclic drying-wetting conditions that result in hysteresis in the SWCC. The soil mechanical behaviour under wetting is crucial since numerous rainfall-induced slope failures occur during the wetting process. However, many slope stability analyses were carried out using drying SWCC. Consequently, the factor of safety (FoS) calculation may not represent the actual field condition. This paper presents the effect of hysteresis in SWCC on the stability of unsaturated residual soil slopes from Bukit Timah Granite in Singapore. The study focused on the analyses considering the differences in pore-water pressure and water content variations under drying and wetting conditions by performing numerical seepage and stability analyses. Each analysis was carried out on a slope subjected to dry and rainy periods under three different conditions: i) using only drying SWCC; ii) using only wetting SWCC; iii) using combined drying and wetting SWCCs. The results indicated that the FoS variations obtained from the numerical analyses incorporating combined SWCC matched more closely those obtained by incorporating only wetting SWCC than those obtained by incorporating only drying SWCC, regardless of the wetting or drying processes that the soil experienced. Moreover, the numerical analyses under high rainfall intensity by incorporating only wetting SWCC gave a more conservative FoS as compared to those obtained by incorporating combined SWCC. Numerical analyses incorporating only drying SWCC gave the most conservative FoS regardless of rainfall intensity. Keywords: SWCC, Hysteresis, Rainfall, Seepage, Slope stability
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spelling doaj.art-fb038731c1804243a1f7a327bc3ea2552024-03-02T17:31:52ZengKeAi Communications Co., Ltd.International Soil and Water Conservation Research2095-63392019-09-0173226238Effect of hysteresis on the stability of residual soil slopeChristofer Kristo0Harianto Rahardjo1Alfrendo Satyanaga2School of Civil and Environmental Engineering, Nanyang Technological University, Hall of Residence 9, Block 46, #04-867, Singapore, 639811, SingaporeCorresponding author.; School of Civil and Environmental Engineering, Nanyang Technological University, Hall of Residence 9, Block 46, #04-867, Singapore, 639811, SingaporeSchool of Civil and Environmental Engineering, Nanyang Technological University, Hall of Residence 9, Block 46, #04-867, Singapore, 639811, SingaporeSoil-water characteristic curve (SWCC) is an essential parameter in unsaturated soil mechanics. Matric suction in unsaturated residual soils changes with varying climatic conditions associated with cyclic drying-wetting conditions that result in hysteresis in the SWCC. The soil mechanical behaviour under wetting is crucial since numerous rainfall-induced slope failures occur during the wetting process. However, many slope stability analyses were carried out using drying SWCC. Consequently, the factor of safety (FoS) calculation may not represent the actual field condition. This paper presents the effect of hysteresis in SWCC on the stability of unsaturated residual soil slopes from Bukit Timah Granite in Singapore. The study focused on the analyses considering the differences in pore-water pressure and water content variations under drying and wetting conditions by performing numerical seepage and stability analyses. Each analysis was carried out on a slope subjected to dry and rainy periods under three different conditions: i) using only drying SWCC; ii) using only wetting SWCC; iii) using combined drying and wetting SWCCs. The results indicated that the FoS variations obtained from the numerical analyses incorporating combined SWCC matched more closely those obtained by incorporating only wetting SWCC than those obtained by incorporating only drying SWCC, regardless of the wetting or drying processes that the soil experienced. Moreover, the numerical analyses under high rainfall intensity by incorporating only wetting SWCC gave a more conservative FoS as compared to those obtained by incorporating combined SWCC. Numerical analyses incorporating only drying SWCC gave the most conservative FoS regardless of rainfall intensity. Keywords: SWCC, Hysteresis, Rainfall, Seepage, Slope stabilityhttp://www.sciencedirect.com/science/article/pii/S2095633918300789
spellingShingle Christofer Kristo
Harianto Rahardjo
Alfrendo Satyanaga
Effect of hysteresis on the stability of residual soil slope
International Soil and Water Conservation Research
title Effect of hysteresis on the stability of residual soil slope
title_full Effect of hysteresis on the stability of residual soil slope
title_fullStr Effect of hysteresis on the stability of residual soil slope
title_full_unstemmed Effect of hysteresis on the stability of residual soil slope
title_short Effect of hysteresis on the stability of residual soil slope
title_sort effect of hysteresis on the stability of residual soil slope
url http://www.sciencedirect.com/science/article/pii/S2095633918300789
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