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Seismic Observations of Fluvial Energy Dissipation

dc.contributor.advisorPrestegaard, Karenen_US
dc.contributor.advisorLekic, Vedranen_US
dc.contributor.authorGoodling, Phillip Jamesen_US
dc.date.accessioned2019-02-01T06:42:23Z
dc.date.available2019-02-01T06:42:23Z
dc.date.issued2018en_US
dc.identifierhttps://doi.org/10.13016/jzfl-qjgl
dc.identifier.urihttp://hdl.handle.net/1903/21661
dc.description.abstractObserving microseismic waves excited by turbulent flow is an emerging way to document river dynamics during extreme flood events. This thesis records fluvial-seismic observations in two contrasting systems at different scales. Two single-seismometer particle motion methods are introduced to characterize the seismic signal produced by rivers. In the large-scale system, the Oroville Dam spillway is observed when it is a simple rectangular channel and when it is damaged by erosion. The small-scale system is along the cobble-bed Northwest Branch of the Anacostia River. Particle motion analyses and the scaling between seismic power and discharge are suitable to characterize flow turbulence at the large-scale system. In the small-scale system, particle motion methods are found to be unsuitable and the scaling of seismic power is unable to resolve observed variability in flow dynamics within the study reach. This work suggests that methods of fluvial seismology are best suited to large-scale systems.en_US
dc.language.isoenen_US
dc.titleSeismic Observations of Fluvial Energy Dissipationen_US
dc.typeThesisen_US
dc.contributor.publisherDigital Repository at the University of Marylanden_US
dc.contributor.publisherUniversity of Maryland (College Park, Md.)en_US
dc.contributor.departmentGeologyen_US
dc.subject.pqcontrolledGeophysicsen_US
dc.subject.pqcontrolledGeomorphologyen_US
dc.subject.pquncontrolledFluvial Seismologyen_US
dc.subject.pquncontrolledHydrodynamicsen_US
dc.subject.pquncontrolledOroville Damen_US
dc.subject.pquncontrolledPolarization Analysisen_US


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