Laboratory Modeling of Critical Hydraulic Conditions for the Initiation of Piping

Seepage-related erosion is one of the predominant mechanisms responsible for incidents and failures of dams and levees. Current geotechnical engineering practice consists of comparing expected exit gradients with the critical gradient of the soil at the seepage exit point. The critical gradient is g...

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Main Author: Fleshman, Mandie Swainston
Format: Others
Published: DigitalCommons@USU 2012
Subjects:
Online Access:https://digitalcommons.usu.edu/etd/1364
https://digitalcommons.usu.edu/cgi/viewcontent.cgi?article=2369&context=etd
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spelling ndltd-UTAHS-oai-digitalcommons.usu.edu-etd-23692019-10-13T06:14:46Z Laboratory Modeling of Critical Hydraulic Conditions for the Initiation of Piping Fleshman, Mandie Swainston Seepage-related erosion is one of the predominant mechanisms responsible for incidents and failures of dams and levees. Current geotechnical engineering practice consists of comparing expected exit gradients with the critical gradient of the soil at the seepage exit point. The critical gradient is generally considered as the ratio of soil buoyant unit weight and the unit weight of water, suggesting that the critical gradient only depends on the void ratio and specific gravity of the solids. However, in the field and in research, it has been observed that piping can initiate at average gradients much lower than unity due to concentrations in flow and non-vertical exit faces. Therefore, there is a need for deeper understanding of the granular scale mechanisms of the piping erosion process. This thesis presents the results of a laboratory study to assess the effects that soil properties and exit face configurations have on the potential for initiation of piping and the piping mechanisms. By using a laboratory device designed and constructed specifically for this study, the critical gradients needed to initiate piping in a variety of sandy soils were measured to assess the effects that parameters such as gradation, grain size, and grain shape have on the critical gradients. The tests are also used to observe the grain scale mechanisms of piping erosion initiation. The ultimate goal of the study is to develop an empirical, but mechanism-based, grain-scale model that can take into account the effects of converging flows, non-horizontal exit faces, and soil properties while assessing the potential for piping erosion to occur. 2012-12-01T08:00:00Z text application/pdf https://digitalcommons.usu.edu/etd/1364 https://digitalcommons.usu.edu/cgi/viewcontent.cgi?article=2369&context=etd Copyright for this work is held by the author. Transmission or reproduction of materials protected by copyright beyond that allowed by fair use requires the written permission of the copyright owners. Works not in the public domain cannot be commercially exploited without permission of the copyright owner. Responsibility for any use rests exclusively with the user. For more information contact Andrew Wesolek (andrew.wesolek@usu.edu). All Graduate Theses and Dissertations DigitalCommons@USU critical gradient hydraulic gradient dam failure internal erosion piping seepage Civil and Environmental Engineering
collection NDLTD
format Others
sources NDLTD
topic critical gradient
hydraulic gradient
dam failure
internal erosion
piping
seepage
Civil and Environmental Engineering
spellingShingle critical gradient
hydraulic gradient
dam failure
internal erosion
piping
seepage
Civil and Environmental Engineering
Fleshman, Mandie Swainston
Laboratory Modeling of Critical Hydraulic Conditions for the Initiation of Piping
description Seepage-related erosion is one of the predominant mechanisms responsible for incidents and failures of dams and levees. Current geotechnical engineering practice consists of comparing expected exit gradients with the critical gradient of the soil at the seepage exit point. The critical gradient is generally considered as the ratio of soil buoyant unit weight and the unit weight of water, suggesting that the critical gradient only depends on the void ratio and specific gravity of the solids. However, in the field and in research, it has been observed that piping can initiate at average gradients much lower than unity due to concentrations in flow and non-vertical exit faces. Therefore, there is a need for deeper understanding of the granular scale mechanisms of the piping erosion process. This thesis presents the results of a laboratory study to assess the effects that soil properties and exit face configurations have on the potential for initiation of piping and the piping mechanisms. By using a laboratory device designed and constructed specifically for this study, the critical gradients needed to initiate piping in a variety of sandy soils were measured to assess the effects that parameters such as gradation, grain size, and grain shape have on the critical gradients. The tests are also used to observe the grain scale mechanisms of piping erosion initiation. The ultimate goal of the study is to develop an empirical, but mechanism-based, grain-scale model that can take into account the effects of converging flows, non-horizontal exit faces, and soil properties while assessing the potential for piping erosion to occur.
author Fleshman, Mandie Swainston
author_facet Fleshman, Mandie Swainston
author_sort Fleshman, Mandie Swainston
title Laboratory Modeling of Critical Hydraulic Conditions for the Initiation of Piping
title_short Laboratory Modeling of Critical Hydraulic Conditions for the Initiation of Piping
title_full Laboratory Modeling of Critical Hydraulic Conditions for the Initiation of Piping
title_fullStr Laboratory Modeling of Critical Hydraulic Conditions for the Initiation of Piping
title_full_unstemmed Laboratory Modeling of Critical Hydraulic Conditions for the Initiation of Piping
title_sort laboratory modeling of critical hydraulic conditions for the initiation of piping
publisher DigitalCommons@USU
publishDate 2012
url https://digitalcommons.usu.edu/etd/1364
https://digitalcommons.usu.edu/cgi/viewcontent.cgi?article=2369&context=etd
work_keys_str_mv AT fleshmanmandieswainston laboratorymodelingofcriticalhydraulicconditionsfortheinitiationofpiping
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