Bed sediment transport and channel morphology in a braided channel: insights from a flume experiment
| dc.contributor.author | Armstrong, Dylan L., author | |
| dc.contributor.author | Ettema, Robert, advisor | |
| dc.contributor.author | Nelson, Peter, committee member | |
| dc.contributor.author | Falkowski, Michael, committee member | |
| dc.date.accessioned | 2017-06-09T15:42:56Z | |
| dc.date.available | 2017-06-09T15:42:56Z | |
| dc.date.issued | 2017 | |
| dc.description.abstract | This thesis presents the methods and findings from an experiment aimed at relating the rate of bed-sediment transport through a reach of a braided channel to the intensity of the braiding sub-channels (anabranches) along the reach. The experiment was conducted in a large flume located at Colorado State University's Hydraulics Laboratory in Fort Collins, Colorado. No similar flume experiments have been conducted involving braided channels in a wide alluvial plain. Such experiments involve several challenging considerations that greatly complicate such experiments: braided channels are characteristically wide and shallow; have relatively large bed-sediment loads that are difficult to measure, because they move in multiple sub-channels; and the sub-channels (often termed anabranches) are ephemeral. The self-forming nature of the anabranches means that there is little direct control over the exact morphology of the braided channel. The objectives set forth in this experiment overcame the challenges of braided river flume studies, and allowed a comprehensive data set to be obtained of both bed sediment transport data and morphologic braided intensity data. The intensity of braiding was characterized using a braiding index (Flow Width Ratio) developed during this experiment. A relationship was identified and a trend established – as FWR increased, the rate of bed-sediment transport decreased – but the stochastic nature of transport rates and morphology introduced much scatter in the relationship. It was found that local morphologic features have a large impact on the transport of sediment through braided systems, and that the features could help explain some of the scatter in the data. | |
| dc.format.medium | born digital | |
| dc.format.medium | masters theses | |
| dc.identifier | Armstrong_colostate_0053N_14174.pdf | |
| dc.identifier.uri | http://hdl.handle.net/10217/181441 | |
| dc.language | English | |
| dc.language.iso | eng | |
| dc.publisher | Colorado State University. Libraries | |
| dc.relation.ispartof | 2000-2019 | |
| dc.rights | Copyright 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.subject | flume study | |
| dc.subject | sediment transport | |
| dc.subject | morphology | |
| dc.subject | braided channel | |
| dc.title | Bed sediment transport and channel morphology in a braided channel: insights from a flume experiment | |
| dc.type | Text | |
| dcterms.rights.dpla | This 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.discipline | Civil and Environmental Engineering | |
| thesis.degree.grantor | Colorado State University | |
| thesis.degree.level | Masters | |
| thesis.degree.name | Master of Science (M.S.) |
Files
Original bundle
1 - 1 of 1
Loading...
- Name:
- Armstrong_colostate_0053N_14174.pdf
- Size:
- 3.64 MB
- Format:
- Adobe Portable Document Format