Stability analysis of unsaturated slopes subjected to rainfall infiltration

Prolonged high intensity rainfall which took place on 17 to 20 December has triggered a number of slope failures at Universiti Teknologi Malaysia (UTM) Skudai campus. Two instrumented slopes were investigated for the effects of soil characteristics on the mechanism of rainfall infiltration in slope....

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Main Authors: El-Fadil, Mohamed El-Byhagi, Gofar, Nurly
Format: Article
Language:English
Published: Faculty of Civil Engineering 2008
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Online Access:http://eprints.utm.my/id/eprint/8582/1/MEBEFadil2008-Stability_Analysis_Of_Unsaturated_Slopes.pdf
http://eprints.utm.my/id/eprint/8582/
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spelling my.utm.85822017-10-19T00:32:59Z http://eprints.utm.my/id/eprint/8582/ Stability analysis of unsaturated slopes subjected to rainfall infiltration El-Fadil, Mohamed El-Byhagi Gofar, Nurly TA Engineering (General). Civil engineering (General) Prolonged high intensity rainfall which took place on 17 to 20 December has triggered a number of slope failures at Universiti Teknologi Malaysia (UTM) Skudai campus. Two instrumented slopes were investigated for the effects of soil characteristics on the mechanism of rainfall infiltration in slope. One slope (Site-1) failed due to the rainfall on the 20th December 2006 while the other (Site- 2) remained stable. With other conditions deemed to be equal, the slope failure at Site-1 was predicted to be caused by the behavior of the soil forming the slope. Analysis showed that for Site 1, the continuous rainfall has caused a significant increase in soil’s moisture, decrease in negative pore-water pressure (from 28 kPa to 0), and hence reduction in the factor of safety (FOS) of the slope from 2.15 to 0.99 for slip plane at depth of 1.8 m. On the other hand, the same rainfall induces a very small change in negative pore-water pressure, and hence reduces the minimum FOS of slope at Site 2 from 3.34 to 2.78. The results showed that the permeability of the soil mass plays an important role in the slope instability; hence more attention should be given to the fine-grained soil slope during monsoon season. Comparison between predicted FOS based on SWCC curve and actual measurement showed that there are other factors that may influence the soil response to rainfall infiltration such as mineralogy of the clay content and the dispersibility of the soil. Faculty of Civil Engineering 2008 Article PeerReviewed application/pdf en http://eprints.utm.my/id/eprint/8582/1/MEBEFadil2008-Stability_Analysis_Of_Unsaturated_Slopes.pdf El-Fadil, Mohamed El-Byhagi and Gofar, Nurly (2008) Stability analysis of unsaturated slopes subjected to rainfall infiltration. Geotechnical & Highway Engineering . http://www.fka.utm.my
institution Universiti Teknologi Malaysia
building UTM Library
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Teknologi Malaysia
content_source UTM Institutional Repository
url_provider http://eprints.utm.my/
language English
topic TA Engineering (General). Civil engineering (General)
spellingShingle TA Engineering (General). Civil engineering (General)
El-Fadil, Mohamed El-Byhagi
Gofar, Nurly
Stability analysis of unsaturated slopes subjected to rainfall infiltration
description Prolonged high intensity rainfall which took place on 17 to 20 December has triggered a number of slope failures at Universiti Teknologi Malaysia (UTM) Skudai campus. Two instrumented slopes were investigated for the effects of soil characteristics on the mechanism of rainfall infiltration in slope. One slope (Site-1) failed due to the rainfall on the 20th December 2006 while the other (Site- 2) remained stable. With other conditions deemed to be equal, the slope failure at Site-1 was predicted to be caused by the behavior of the soil forming the slope. Analysis showed that for Site 1, the continuous rainfall has caused a significant increase in soil’s moisture, decrease in negative pore-water pressure (from 28 kPa to 0), and hence reduction in the factor of safety (FOS) of the slope from 2.15 to 0.99 for slip plane at depth of 1.8 m. On the other hand, the same rainfall induces a very small change in negative pore-water pressure, and hence reduces the minimum FOS of slope at Site 2 from 3.34 to 2.78. The results showed that the permeability of the soil mass plays an important role in the slope instability; hence more attention should be given to the fine-grained soil slope during monsoon season. Comparison between predicted FOS based on SWCC curve and actual measurement showed that there are other factors that may influence the soil response to rainfall infiltration such as mineralogy of the clay content and the dispersibility of the soil.
format Article
author El-Fadil, Mohamed El-Byhagi
Gofar, Nurly
author_facet El-Fadil, Mohamed El-Byhagi
Gofar, Nurly
author_sort El-Fadil, Mohamed El-Byhagi
title Stability analysis of unsaturated slopes subjected to rainfall infiltration
title_short Stability analysis of unsaturated slopes subjected to rainfall infiltration
title_full Stability analysis of unsaturated slopes subjected to rainfall infiltration
title_fullStr Stability analysis of unsaturated slopes subjected to rainfall infiltration
title_full_unstemmed Stability analysis of unsaturated slopes subjected to rainfall infiltration
title_sort stability analysis of unsaturated slopes subjected to rainfall infiltration
publisher Faculty of Civil Engineering
publishDate 2008
url http://eprints.utm.my/id/eprint/8582/1/MEBEFadil2008-Stability_Analysis_Of_Unsaturated_Slopes.pdf
http://eprints.utm.my/id/eprint/8582/
http://www.fka.utm.my
_version_ 1643645025457799168
score 13.159267