The Exchange of Fine Muddy Sediment in Gravel-Bed Fluvial Systems
| dc.contributor.author | Schiller, Brayden Jeffery | en |
| dc.contributor.committeechair | Strom, Kyle Brent | en |
| dc.contributor.committeemember | Hester, Erich Todd | en |
| dc.contributor.committeemember | Frimpong, Emmanuel Anokye | en |
| dc.contributor.department | Civil and Environmental Engineering | en |
| dc.date.accessioned | 2024-06-01T08:03:29Z | en |
| dc.date.available | 2024-06-01T08:03:29Z | en |
| dc.date.issued | 2024-05-31 | en |
| dc.description.abstract | The presence of fine muddy sediment (grain size < 0.1 mm) in streams has many impacts on the fluvial system and those relying on it, both humans and aquatic biota. Previously, fine sediment was considered a washload and has been ignored in transport models. More recently, it has been treated as being transported once the surface gravel layer that stores it is able to be mobilized. We propose that the surface layer need not be mobilized in order for muddy sediment to travel through the fluvial system in a series of erosive and depositional events. Our first study uses a new in situ device to show how mud entrainment from immobile gravel beds behaves cohesionlessly and can be modeled using the framework of classic sand-based models modified to account for hiding effects present in the stream bed. It also provides a method to predict how deep into the surface layer of gravel entrainment of fine sediment will occur given flow and stream bed characteristics. The second study investigates the primary pathway that fine sediment is traveling to get captured within bluehead chub fish nests. It was determined that more deposition of mud occurred in the upstream half of the nest concluding that the primary pathway was hyporheic pumping through the nest. Capture efficiencies of the nests were also found to increase as the length of nests increased. Both of these studies provide supporting evidence in the need to transition modeling fine sediment transport as a series of deposition and resuspension. | en |
| dc.description.abstractgeneral | Fine muddy sediment (grain size < 0.1 mm) is present in natural streams and has many impacts on the stream system and those relying on it, including humans, plants, animals, and other organisms in the ecosystem. Previously, fine sediment was treated as being too small to consider in models that aid in understanding how a stream transports sediment. This is because small sediment stays suspended in the water column more easily than larger sediment. Therefore, it was just assumed to pass through the system and never deposit into the stream bed. However, in nature we observe large quantities of fine sediment being stored within the stream bed. More recently, it has been assumed that the sediment that does deposit will be transported once the surface gravel layer that stores it is able to be mobilized. That is, the surface gravel layer shields the fine sediment trapped between it and that the mud will stay put until that gravel is moved. We propose that the surface layer need not be mobilized for muddy sediment to travel through the fluvial system in a series of erosive and depositional events. Our first study uses a new device that forces erosion of mud to show how mud entrainment, or the process of how a fluid picks something up and carries it, from immobile gravel beds can be modeled using the framework of classic sand-based entrainment models modified to account for hiding effects, or protection against entrainment of a smaller sediment by a larger sediment shielding it, present in the stream bed. It also provides a method to predict how deep into the surface layer of gravel that fine sediment will be eroded given flow and stream bed characteristics. This is beneficial in estimating the amount of sediment that will be eroded during a given storm event. The second study investigates the primary pathway that fine sediment is traveling to get captured within bluehead chub gravel fish nests used for spawning their eggs and reproducing. It was determined that more deposition of mud occurred in the upstream half of the nest. This leads us to believe that the primary pathway of sediment traveling through the nest was hyporheic pumping through the nest, or the process of water flowing down through the surface layers of sediment in the stream bed. Capture efficiencies, or the ratio of how much of the sediment that traveled through the nest was captured, of the nests were also found to increase as the length of nests in the downstream direction increased. Both of these studies provide supporting evidence in the need to transition modeling fine sediment transport as a series of deposition and resuspension. | en |
| dc.description.degree | Master of Science | en |
| dc.format.medium | ETD | en |
| dc.identifier.other | vt_gsexam:40990 | en |
| dc.identifier.uri | https://hdl.handle.net/10919/119219 | en |
| dc.language.iso | en | en |
| dc.publisher | Virginia Tech | en |
| dc.rights | In Copyright | en |
| dc.rights.uri | http://rightsstatements.org/vocab/InC/1.0/ | en |
| dc.subject | fine sediment | en |
| dc.subject | entrainment | en |
| dc.subject | sediment transport | en |
| dc.subject | erosion | en |
| dc.subject | bluehead chub | en |
| dc.subject | spawning nests | en |
| dc.subject | deposition | en |
| dc.subject | siltation | en |
| dc.title | The Exchange of Fine Muddy Sediment in Gravel-Bed Fluvial Systems | en |
| dc.type | Thesis | en |
| thesis.degree.discipline | Civil Engineering | en |
| thesis.degree.grantor | Virginia Polytechnic Institute and State University | en |
| thesis.degree.level | masters | en |
| thesis.degree.name | Master of Science | en |
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