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dc.contributor.authorF. Bressan
dc.contributor.authorA. (Thanos) N. Papanicolaou
dc.contributor.authorJ. T. Thomas
dc.contributor.authorC. G. Wilson
dc.contributor.authorM. Elhakeem
dc.date.accessioned2018-04-05T11:31:49Z
dc.date.available2018-04-05T11:31:49Z
dc.date.issued2013
dc.identifier.citationhttps://ascelibrary-org.adu-lib-database.idm.oclc.org/doi/pdf/10.1061/9780784412947.193en_US
dc.identifier.urihttps://dspace.adu.ac.ae/handle/1/1065
dc.descriptionBressan, F., Papanicolaou, A. T. N., Thomas, J. T., Wilson, C. G., & Elhakeem, M. (2013). Knickpoint migration and evolution in the Deep Loess Region of western Iowa. In World Environmental and Water Resources Congress 2013: Showcasing the Future (pp. 1971-1980).
dc.description.abstractKnickpoints are geomorphic bed features characterized by the formation of a sharp change (i.e., knick) in the channel slope leading to the creation of a wide crest staircase. Knickpoints migrate upstream and cause bank instability, exposure of bridge-crossing foundations, and the deterioration of fish habitat. They are a common geomorphic hazard in many streams of the Midwestern United States that is partly due to prevailing management practices, including stream channelization, which mostly occurred during the first half of the 20th century. Over the last 40 years, local governmental agencies have attempted to halt knickpoint migration by constructing different types of grade control structures (GCS). Despite these attempts, the problem still persists. Understanding of the mechanisms triggering the onset of knickpoint migration is at a primitive stage. In this study, a field evaluation of a representative channel reach containing a knickpoint in the Deep Loess Region of western Iowa was used to test current theoretical and numerical models of knickpoint migration. Continuous stage and periodic flow measurements were recorded for almost two years and included an extreme event, which occurred during the catastrophic 2008 Midwestern United States floods. In addition, soil samples from the river bed and banks were collected and the bathymetry was measured to fully characterize the stream reach. The data were used to estimate the parameters of various models to quantify the knickpoint migration rate and evolution during various hydrological events. The final goal of this research is to identify the most suitable approach to model the knickpoints found in Midwestern streams. The results of the study can then be used by federal or state agencies to define better plans for the future control of bed degradation using more adequate GCS.en_US
dc.language.isoen_USen_US
dc.publisherAmerican Society of Civil Engineersen_US
dc.subjectBridge foundationsen_US
dc.titleKnickpoint Migration and Evolution in the Deep Loess Region of Western Iowaen_US
dc.typeArticleen_US
dc.identifier.doihttps://doi.org/10.1061/9780784412947.193


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