Correlation of acoustic emissions with patterns of movement in an extremely slow moving landslide at Peace River, Alberta, Canada

The Peace River region, Alberta, Canada, has experienced extensive landslide activity since deglaciation. Shear zones within weak lacustrine silt and clay layers typically experience continuous creep, damaging highway and utilities infrastructure. However, occasionally, movement accelerates and pote...

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Main Authors: Berg, Nancy, Smith, Alister, Russell, Shawn, Dixon, Neil, Proudfoot, Don, Take, W. Andy
Format: Article in Journal/Newspaper
Language:unknown
Published: NRC Research Press (a division of Canadian Science Publishing) 2017
Subjects:
Online Access:http://hdl.handle.net/1807/90481
http://www.nrcresearchpress.com/doi/abs/10.1139/cgj-2016-0668
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spelling ftunivtoronto:oai:localhost:1807/90481 2023-05-15T17:54:48+02:00 Correlation of acoustic emissions with patterns of movement in an extremely slow moving landslide at Peace River, Alberta, Canada Berg, Nancy Smith, Alister Russell, Shawn Dixon, Neil Proudfoot, Don Take, W. Andy 2017-06-07 http://hdl.handle.net/1807/90481 http://www.nrcresearchpress.com/doi/abs/10.1139/cgj-2016-0668 unknown NRC Research Press (a division of Canadian Science Publishing) 0008-3674 http://hdl.handle.net/1807/90481 http://www.nrcresearchpress.com/doi/abs/10.1139/cgj-2016-0668 Article 2017 ftunivtoronto 2020-06-17T12:20:04Z The Peace River region, Alberta, Canada, has experienced extensive landslide activity since deglaciation. Shear zones within weak lacustrine silt and clay layers typically experience continuous creep, damaging highway and utilities infrastructure. However, occasionally, movement accelerates and potentially catastrophic failures occur. Conventional deformation monitoring approaches provide incremental measurements with low temporal resolution and do not necessarily allow rapid changes in stability to be detected and communicated sufficiently in advance to provide early warning. The study objectives were to (i) acquire a long-term dataset of continuous deformation measurements with high temporal resolution of a case study slope in Peace River, (ii) enhance understanding of a typical creeping Peace River slope’s behavior in response to climatic drivers, and (iii) investigate the potential of an acoustic emission (AE) monitoring system to provide early warning of accelerating deformation behavior. ShapeAccelArray (SAA) and AE instruments were installed, in addition to conventional inclinometers and piezometers. Measurements show that the landslide is “extremely slow”, moving on average 5 mm annually, and reveal seasonal activity with periods of acceleration and deceleration driven by pore-water pressures. Measured AE correlated strongly with the rate and magnitude of SAA-measured displacement, demonstrating the potential of the AE technique to warn of accelerating deformation behavior. The accepted manuscript in pdf format is listed with the files at the bottom of this page. The presentation of the authors' names and (or) special characters in the title of the manuscript may differ slightly between what is listed on this page and what is listed in the pdf file of the accepted manuscript; that in the pdf file of the accepted manuscript is what was submitted by the author. Article in Journal/Newspaper Peace River University of Toronto: Research Repository T-Space Canada
institution Open Polar
collection University of Toronto: Research Repository T-Space
op_collection_id ftunivtoronto
language unknown
description The Peace River region, Alberta, Canada, has experienced extensive landslide activity since deglaciation. Shear zones within weak lacustrine silt and clay layers typically experience continuous creep, damaging highway and utilities infrastructure. However, occasionally, movement accelerates and potentially catastrophic failures occur. Conventional deformation monitoring approaches provide incremental measurements with low temporal resolution and do not necessarily allow rapid changes in stability to be detected and communicated sufficiently in advance to provide early warning. The study objectives were to (i) acquire a long-term dataset of continuous deformation measurements with high temporal resolution of a case study slope in Peace River, (ii) enhance understanding of a typical creeping Peace River slope’s behavior in response to climatic drivers, and (iii) investigate the potential of an acoustic emission (AE) monitoring system to provide early warning of accelerating deformation behavior. ShapeAccelArray (SAA) and AE instruments were installed, in addition to conventional inclinometers and piezometers. Measurements show that the landslide is “extremely slow”, moving on average 5 mm annually, and reveal seasonal activity with periods of acceleration and deceleration driven by pore-water pressures. Measured AE correlated strongly with the rate and magnitude of SAA-measured displacement, demonstrating the potential of the AE technique to warn of accelerating deformation behavior. The accepted manuscript in pdf format is listed with the files at the bottom of this page. The presentation of the authors' names and (or) special characters in the title of the manuscript may differ slightly between what is listed on this page and what is listed in the pdf file of the accepted manuscript; that in the pdf file of the accepted manuscript is what was submitted by the author.
format Article in Journal/Newspaper
author Berg, Nancy
Smith, Alister
Russell, Shawn
Dixon, Neil
Proudfoot, Don
Take, W. Andy
spellingShingle Berg, Nancy
Smith, Alister
Russell, Shawn
Dixon, Neil
Proudfoot, Don
Take, W. Andy
Correlation of acoustic emissions with patterns of movement in an extremely slow moving landslide at Peace River, Alberta, Canada
author_facet Berg, Nancy
Smith, Alister
Russell, Shawn
Dixon, Neil
Proudfoot, Don
Take, W. Andy
author_sort Berg, Nancy
title Correlation of acoustic emissions with patterns of movement in an extremely slow moving landslide at Peace River, Alberta, Canada
title_short Correlation of acoustic emissions with patterns of movement in an extremely slow moving landslide at Peace River, Alberta, Canada
title_full Correlation of acoustic emissions with patterns of movement in an extremely slow moving landslide at Peace River, Alberta, Canada
title_fullStr Correlation of acoustic emissions with patterns of movement in an extremely slow moving landslide at Peace River, Alberta, Canada
title_full_unstemmed Correlation of acoustic emissions with patterns of movement in an extremely slow moving landslide at Peace River, Alberta, Canada
title_sort correlation of acoustic emissions with patterns of movement in an extremely slow moving landslide at peace river, alberta, canada
publisher NRC Research Press (a division of Canadian Science Publishing)
publishDate 2017
url http://hdl.handle.net/1807/90481
http://www.nrcresearchpress.com/doi/abs/10.1139/cgj-2016-0668
geographic Canada
geographic_facet Canada
genre Peace River
genre_facet Peace River
op_relation 0008-3674
http://hdl.handle.net/1807/90481
http://www.nrcresearchpress.com/doi/abs/10.1139/cgj-2016-0668
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