The influence of slope geology on landslide occurrence during extreme rainfall
The influence of slope geology on landslide occurrence during extreme rainfall
Extreme rainfall events, seasonal weather extremes and long term climate change present a threat to the stability of natural and engineered slopes by altering slope hydrology and shear strength beyond recent historical values. The temporal and spatial fluctuation of slope wetting and drying in response to weather event sequences can be represented using a surface water balance approach of rainfall infiltration and potential evapotranspiration, such as a soil moisture deficit calculation (SMD). This provides an opportunity to address the regional susceptibility of slopes to become unstable when exposed to adverse weather event sequences. However, case studies have shown that site specific characterisation of foundation geology (e.g. permeability and shear strength) is required to assess the vulnerability of specific slopes to pore water pressure fluctuations and slope failure during extreme weather events. The relationship between underlying geology and landslide incidence during extreme weather extremes is illustrated by comparing long term weather data, soil moisture deficit calculations and geological information using a database of over 400 UK landslide events that occurred between 2004 and 2014.
1813 - 1818
Muddle, D.
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Briggs, K.M.
8974f7ce-2757-4481-9dbc-07510b416de4
Dashwood, C.
8f665f97-1188-4cc3-be9c-a02af9e1445b
Dijkstra, T.
76b72925-d387-4ee4-9995-4df18b414d1d
2015
Muddle, D.
56a6eab7-9378-45c8-b679-1a16d7e9f724
Briggs, K.M.
8974f7ce-2757-4481-9dbc-07510b416de4
Dashwood, C.
8f665f97-1188-4cc3-be9c-a02af9e1445b
Dijkstra, T.
76b72925-d387-4ee4-9995-4df18b414d1d
Muddle, D., Briggs, K.M., Dashwood, C. and Dijkstra, T.
(2015)
The influence of slope geology on landslide occurrence during extreme rainfall.
In Geotechnical Engineering for Infrastructure and Development - Proceedings of the XVI European Conference on Soil Mechanics and Geotechnical Engineering, ECSMGE 2015.
vol. 4,
ICE Publishing.
.
Record type:
Conference or Workshop Item
(Paper)
Abstract
Extreme rainfall events, seasonal weather extremes and long term climate change present a threat to the stability of natural and engineered slopes by altering slope hydrology and shear strength beyond recent historical values. The temporal and spatial fluctuation of slope wetting and drying in response to weather event sequences can be represented using a surface water balance approach of rainfall infiltration and potential evapotranspiration, such as a soil moisture deficit calculation (SMD). This provides an opportunity to address the regional susceptibility of slopes to become unstable when exposed to adverse weather event sequences. However, case studies have shown that site specific characterisation of foundation geology (e.g. permeability and shear strength) is required to assess the vulnerability of specific slopes to pore water pressure fluctuations and slope failure during extreme weather events. The relationship between underlying geology and landslide incidence during extreme weather extremes is illustrated by comparing long term weather data, soil moisture deficit calculations and geological information using a database of over 400 UK landslide events that occurred between 2004 and 2014.
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Published date: 2015
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Local EPrints ID: 493737
URI: http://eprints.soton.ac.uk/id/eprint/493737
PURE UUID: ef26eaff-5489-4f4d-b073-affd707661d1
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Date deposited: 11 Sep 2024 17:25
Last modified: 14 Sep 2024 01:43
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Contributors
Author:
D. Muddle
Author:
K.M. Briggs
Author:
C. Dashwood
Author:
T. Dijkstra
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