Field monitoring of soil-moisture to understand the hydrological response of a road-cut slope

Rainfall and slope-cutting for road construction are two key landslide causative factors in Nepal, but how they interact to cause failures is poorly understood. To improve understanding of the effects of cut slopes during rainfall, geotechnical investigations and field monitoring were conducted in a...

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Main Authors: Pradhan Samprada, Toll David G., Rosser Nick J., Brain Matthew J.
Format: Article
Language:English
Published: EDP Sciences 2020-01-01
Series:E3S Web of Conferences
Online Access:https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/55/e3sconf_e-unsat2020_01029.pdf
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spelling doaj-f4635d5b622243d48374e2128bc955422021-02-02T05:06:43ZengEDP SciencesE3S Web of Conferences2267-12422020-01-011950102910.1051/e3sconf/202019501029e3sconf_e-unsat2020_01029Field monitoring of soil-moisture to understand the hydrological response of a road-cut slopePradhan Samprada0Toll David G.1Rosser Nick J.2Brain Matthew J.3Institute of Hazard, Risk and Resilience, Durham UniversityInstitute of Hazard, Risk and Resilience, Durham UniversityInstitute of Hazard, Risk and Resilience, Durham UniversityInstitute of Hazard, Risk and Resilience, Durham UniversityRainfall and slope-cutting for road construction are two key landslide causative factors in Nepal, but how they interact to cause failures is poorly understood. To improve understanding of the effects of cut slopes during rainfall, geotechnical investigations and field monitoring were conducted in a mountainous district, Sindhupalchowk, located in central Nepal. This paper presents the results of the field-investigations and the measurements of volumetric water content obtained from the sensors installed in the study-site. Field-based evidence suggests that the slope that was cut for road construction during the dry period remained stable due to the presence of soil suction, which imparted additional strength to the soil. At the start of the monsoon, infiltration of rainwater caused saturation of the soil at shallow depth, consequently causing loss of suction and reduction of the soil strength. The presence of the road-cut in the hillslope resulting in steeper slopes then promoted the failure. These observations suggest that the presence of road-cuts in the hillslopes can cause landslides even during non-exceptional rainfall events.https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/55/e3sconf_e-unsat2020_01029.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Pradhan Samprada
Toll David G.
Rosser Nick J.
Brain Matthew J.
spellingShingle Pradhan Samprada
Toll David G.
Rosser Nick J.
Brain Matthew J.
Field monitoring of soil-moisture to understand the hydrological response of a road-cut slope
E3S Web of Conferences
author_facet Pradhan Samprada
Toll David G.
Rosser Nick J.
Brain Matthew J.
author_sort Pradhan Samprada
title Field monitoring of soil-moisture to understand the hydrological response of a road-cut slope
title_short Field monitoring of soil-moisture to understand the hydrological response of a road-cut slope
title_full Field monitoring of soil-moisture to understand the hydrological response of a road-cut slope
title_fullStr Field monitoring of soil-moisture to understand the hydrological response of a road-cut slope
title_full_unstemmed Field monitoring of soil-moisture to understand the hydrological response of a road-cut slope
title_sort field monitoring of soil-moisture to understand the hydrological response of a road-cut slope
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2020-01-01
description Rainfall and slope-cutting for road construction are two key landslide causative factors in Nepal, but how they interact to cause failures is poorly understood. To improve understanding of the effects of cut slopes during rainfall, geotechnical investigations and field monitoring were conducted in a mountainous district, Sindhupalchowk, located in central Nepal. This paper presents the results of the field-investigations and the measurements of volumetric water content obtained from the sensors installed in the study-site. Field-based evidence suggests that the slope that was cut for road construction during the dry period remained stable due to the presence of soil suction, which imparted additional strength to the soil. At the start of the monsoon, infiltration of rainwater caused saturation of the soil at shallow depth, consequently causing loss of suction and reduction of the soil strength. The presence of the road-cut in the hillslope resulting in steeper slopes then promoted the failure. These observations suggest that the presence of road-cuts in the hillslopes can cause landslides even during non-exceptional rainfall events.
url https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/55/e3sconf_e-unsat2020_01029.pdf
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