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Criteria for the formation of sediment plugs in alluvial rivers

dc.contributor.authorBoroughs, Craig B., author
dc.contributor.authorAbt, Steven R., advisor
dc.contributor.authorThornton, Christopher I., committee member
dc.contributor.authorJulien, Pierre Y., committee member
dc.contributor.authorWatson, Chester C., committee member
dc.contributor.authorAnthony, Deborah J., committee member
dc.date.accessioned2026-02-23T19:14:49Z
dc.date.issued2005
dc.description.abstractThere are several documented cases of sediment plug development in alluvial rivers. General qualitative theories have been offered about the cause of plug formation that pertain to such factors as a sudden decline in sediment transport capacity, the effect of debris in a channel, or human factors such as watershed management. These findings are pertinent but do not contribute to the understanding of the specific processes occurring at the location where plugs develop. Site characteristics, processes, and associated parameters regarding sediment plug formation were evaluated based on a comprehensive literature review, evaluation of data, and discussions with other researchers. All of these topics were analyzed for a focus study reach along the Middle Rio Grande in New Mexico to identify consistencies between periods when plugs formed versus periods when plugs did not develop. The topics were also analyzed against information from other river systems where plugs developed. A theory was formulated regarding the cause of plug development. Sediment plugs always occurred in alluvial rivers at the location of a constriction that abruptly forces a significant portion of flow overbank. As flows are lost, sediment transport capacity decreases, but the total sediment load in the main channel does not reduce by the same proportion. As a result, deposition ensues in the main channel. If flows continue to overbank for weeks, the deposition will eventually completely clog the main channel of the river. This theory was tested using a calibrated and validated original sediment transport/movable bed computer model. Criteria for plug formation were developed with the model and tested against a case for plug development and against another scenario when a plug did not form. These criteria can be used to identify critical thresholds for plug development. The level of plug formation (55% of the main channel, 70% of the main channel, etc.) can be determined to a specified level of confidence. River managers not only have a better understanding as to why plugs form in alluvial rivers but will be able to apply these criteria to evaluate scenarios for a site that is prone to plug formation and address the conditions that might lead to plug development.
dc.format.mediumdoctoral dissertations
dc.identifier.urihttps://hdl.handle.net/10217/243293
dc.languageEnglish
dc.language.isoeng
dc.publisherColorado State University. Libraries
dc.relation.ispartof2000-2019
dc.rightsCopyright and other restrictions may apply. User is responsible for compliance with all applicable laws. For information about copyright law, please see https://libguides.colostate.edu/copyright.
dc.rights.licensePer the terms of a contractual agreement, all use of this item is limited to the non-commercial use of Colorado State University and its authorized users.
dc.subjectcivil engineering
dc.subjecthydrology
dc.subjecthydrologic sciences
dc.titleCriteria for the formation of sediment plugs in alluvial rivers
dc.typeText
dcterms.rights.dplaThis Item is protected by copyright and/or related rights (https://rightsstatements.org/vocab/InC/1.0/). You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s).
thesis.degree.disciplineCivil Engineering
thesis.degree.grantorColorado State University
thesis.degree.levelDoctoral
thesis.degree.nameDoctor of Philosophy (Ph.D.)

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