Quantification of acoustic emission from soils for predicting landslide failure

Acoustic emission (AE) is a natural phenomenon that occurs when a solid is subjected to stress. These emissions are produced by all materials during pre failure. In soil, AE results from the release of energy as particles undergo small strains. If these emissions can be detected, then it becomes pos...

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Main Author: Spriggs, M. P.
Published: Loughborough University 2005
Subjects:
Online Access:http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.418387
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spelling ndltd-bl.uk-oai-ethos.bl.uk-4183872015-03-20T04:27:37ZQuantification of acoustic emission from soils for predicting landslide failureSpriggs, M. P.2005Acoustic emission (AE) is a natural phenomenon that occurs when a solid is subjected to stress. These emissions are produced by all materials during pre failure. In soil, AE results from the release of energy as particles undergo small strains. If these emissions can be detected, then it becomes possible to develop an early warning system to predict slope failure. International research has shown that AE can be used to detect ground deformations earlier than traditional techniques, and thus it has a role to play in reducing risk to humans, property and in mitigating such risks. This thesis researches the design of a system to quantify the AE and calculate the distance to the deformation zone, and hence information on the mechanism of movement. The quantification of AE is derived from measuring the AE event rate, the output of which takes the form of a displacement rate. This is accurate to an order of magnitude, in line with current standards for classifying slope movements The system also demonstrates great sensitivity to changes within the displacement rate by an order of magnitude, making the technique suitable to remediation monitoring. Knowledge of the position of the shear surface is critical to the planning of cost effective stabllisation measures. This thesis details the development of a single sensor source location technique used to obtain the depth of a developing or existing shear surface within a slope. The active waveguide is used to reduce attenuation by taking advantage of the relatively low attenuation of metals such as steel. A method of source location based on the analysis of Lamb wave mode arrival times at a smgle sensor is summansed. An automatic approach to source location is demonstrated to locate a regular AE source to within one metre. Overall consideration is also given to field trials and towards the production of monitoring protocols for data analysis, and the implementation of necessary emergency/remediation plans.624.151360287Acoustic emission : Source location : Waveguide : Slope instability : Lamb waves : AE event rateLoughborough Universityhttp://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.418387https://dspace.lboro.ac.uk/2134/10903Electronic Thesis or Dissertation
collection NDLTD
sources NDLTD
topic 624.151360287
Acoustic emission : Source location : Waveguide : Slope instability : Lamb waves : AE event rate
spellingShingle 624.151360287
Acoustic emission : Source location : Waveguide : Slope instability : Lamb waves : AE event rate
Spriggs, M. P.
Quantification of acoustic emission from soils for predicting landslide failure
description Acoustic emission (AE) is a natural phenomenon that occurs when a solid is subjected to stress. These emissions are produced by all materials during pre failure. In soil, AE results from the release of energy as particles undergo small strains. If these emissions can be detected, then it becomes possible to develop an early warning system to predict slope failure. International research has shown that AE can be used to detect ground deformations earlier than traditional techniques, and thus it has a role to play in reducing risk to humans, property and in mitigating such risks. This thesis researches the design of a system to quantify the AE and calculate the distance to the deformation zone, and hence information on the mechanism of movement. The quantification of AE is derived from measuring the AE event rate, the output of which takes the form of a displacement rate. This is accurate to an order of magnitude, in line with current standards for classifying slope movements The system also demonstrates great sensitivity to changes within the displacement rate by an order of magnitude, making the technique suitable to remediation monitoring. Knowledge of the position of the shear surface is critical to the planning of cost effective stabllisation measures. This thesis details the development of a single sensor source location technique used to obtain the depth of a developing or existing shear surface within a slope. The active waveguide is used to reduce attenuation by taking advantage of the relatively low attenuation of metals such as steel. A method of source location based on the analysis of Lamb wave mode arrival times at a smgle sensor is summansed. An automatic approach to source location is demonstrated to locate a regular AE source to within one metre. Overall consideration is also given to field trials and towards the production of monitoring protocols for data analysis, and the implementation of necessary emergency/remediation plans.
author Spriggs, M. P.
author_facet Spriggs, M. P.
author_sort Spriggs, M. P.
title Quantification of acoustic emission from soils for predicting landslide failure
title_short Quantification of acoustic emission from soils for predicting landslide failure
title_full Quantification of acoustic emission from soils for predicting landslide failure
title_fullStr Quantification of acoustic emission from soils for predicting landslide failure
title_full_unstemmed Quantification of acoustic emission from soils for predicting landslide failure
title_sort quantification of acoustic emission from soils for predicting landslide failure
publisher Loughborough University
publishDate 2005
url http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.418387
work_keys_str_mv AT spriggsmp quantificationofacousticemissionfromsoilsforpredictinglandslidefailure
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