Long-term geoelectrical monitoring of landslides in natural and engineered slopes

Author:

Chambers Jonathan1,Holmes Jessica2,Whiteley Jim1,Boyd James13,Meldrum Philip1,Wilkinson Paul1,Kuras Oliver1,Swift Russell14,Harrison Harry1,Glendinning Stephanie2,Stirling Ross2,Huntley David5,Slater Nick6,Donohue Shane7

Affiliation:

1. British Geological Survey, Nottingham, UK..

2. Newcastle University, Newcastle upon Tyne, UK..

3. Lancaster University, Lancaster, UK.

4. University of Liège, Liège, Belgium.

5. Geological Survey of Canada, Vancouver, British Columbia, Canada..

6. Socotec Monitoring Ltd., East Sussex, UK..

7. University College Dublin, Dublin, Ireland..

Abstract

Developments in time-lapse electrical resistivity tomography (ERT) technology are transforming our ability to monitor the subsurface due to purpose-built monitoring instruments, advances in automation and modeling, and the resulting improvements in spatial and temporal resolution. We describe the development of a novel ERT-based remote monitoring system called PRIME that integrates new low-power measurement instrumentation with data delivery, automated data processing and image generation, and web-based information delivery. Due to the sensitivity of ERT to hydrologic processes in the near surface, we focus on the application of PRIME for moisture-driven landslide monitoring. Case examples are considered of landslides in engineered and natural slopes, including those impacting geotechnical assets in rail and highways, where slope hydrology is seen to be controlled by lithology, vegetation, fissuring, and drainage structures. We conclude by taking a forward look at emerging developments in ERT monitoring relating to hardware, software and modeling, and applications.

Funder

Research Councils UK

Publisher

Society of Exploration Geophysicists

Subject

Geology,Geophysics

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5. Hobbs, P. R. N., D. C. Entwisle, K. J. Northmore, M. G. Sumbler, L. D. Jones, S. Kemp, S. Self et al. 2005, The engineering geology of UK rocks and soils: The Lias Group, British Geological Survey Internal Report, IR/05/008.

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