Abstract

Observations show that many soils in linear geotechnical infrastructure including embankments and cuttings undergo seasonal volume changes, and different studies confirm that this is due to cycles in climatic and hydrological conditions. These cycles can give rise to progressive failure of the soil mass, which in turn may lead to deterioration of performance and ultimately slope failure. It is expected that the magnitude of the seasonal cycles of pore pressure will be increased by more extreme and more frequent events of wet and dry periods predicted by future climate scenarios. In this paper, numerical modelling has been undertaken to simulate a continuous time series pore water pressure within a representative cutting in London Clay. The approach uses synthetic control and future climate scenarios from a weather generator to investigate the potential impacts of climate change on cutting stability. Surface pore water pressures are obtained by a hydrological model, which are then applied to a coupled fluid-mechanical model. These models are able to capture the significant soil–vegetation–atmospheric interaction processes allowing the induced unsaturated hydro-mechanical response to be investigated. The chosen hydraulic conductivity variables in the model are shown to affect the total magnitude of pore pressure fluctuation and hence the rate of progressive failure. The results demonstrate for the first time that higher total magnitude of annual variation in pore pressures caused by future climate scenarios can have a significant effect on deformations in cuttings. This in turn leads to increased rates of deterioration and reduces time to failure.

Highlights

  • There is agreement within the scientific community that the climate is changing and those changes have been quantified for a number of scenarios within the UK [36, 38]

  • The results demonstrate for the first time that higher total magnitude of annual variation in pore pressures caused by future climate scenarios can have a significant effect on deformations in cuttings

  • A methodology has been described for modelling the progressive failure of a cut slope due to fluctuations in pore water pressure as driven by meteorological boundary conditions

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Summary

Introduction

There is agreement within the scientific community that the climate is changing and those changes have been quantified for a number of scenarios within the UK [36, 38]. Natural slopes and infrastructure cuttings constructed within a clay material are susceptible to seasonal changes in pore water pressures during infiltration These changes have been continuously monitored by a number of authors [14, 34, 56, 61, 67, 69]. The effect of changing vegetation on stability during the lifecycle of slopes has been investigated, demonstrating that vegetation contributes to increased stability due to rooting reinforcement and the generation of large suctions, this in turn can negatively impact serviceability [8, 32, 49, 70] These modelled results are supported by field observations [10]. The effects of the synthetic climate on pore water pressure cycles and subsequent changes in effective stress are modelled in order to investigate the rate of deterioration due to progressive failure and how this process is likely to be exacerbated in the future

Modelling strategy
Hydrological model
Mechanical model
Climate scenarios
Model validation
Hydrological model validation
Initial conditions for the hydrological validation model
Mechanical model validation
Application of the control and future scenarios to the cut slope model
Modelling scenarios
Pore water pressures
Mechanical response
The effect of hydraulic conductivity on cut slope stability
Findings
Conclusion
Full Text
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