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dc.contributor.authorBirchler, Justin J.  Concept link
dc.contributor.authorHarris, Courtney K.  Concept link
dc.contributor.authorSherwood, Christopher R.  Concept link
dc.contributor.authorKniskern, Tara A.  Concept link
dc.date.accessioned2019-02-07T17:07:56Z
dc.date.available2019-02-07T17:07:56Z
dc.date.issued2018-11-27
dc.identifier.citationBirchler, J. J., Harris, C. K., Sherwood, C. R., & Kniskern, T. A. (2018). Sediment transport model including short-lived radioisotopes: Model description and idealized test cases. Journal of Marine Science and Engineering, 6(4), 144en_US
dc.identifier.urihttps://hdl.handle.net/1912/23638
dc.descriptionAuthor Posting. © American Meteorological Society, 2018. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Marine Science and Engineering 6(4), (2018): 144. doi:10.3390/jmse6040144.en_US
dc.description.abstractGeochronologies derived from sediment cores in coastal locations are often used to infer event bed characteristics such as deposit thicknesses and accumulation rates. Such studies commonly use naturally occurring, short-lived radioisotopes, such as Beryllium-7 (7Be) and Thorium-234 (234Th), to study depositional and post-depositional processes. These radioisotope activities, however, are not generally represented in sediment transport models that characterize coastal flood and storm deposition with grain size patterns and deposit thicknesses. We modified the Community Sediment Transport Modeling System (CSTMS) to account for reactive tracers and used this capability to represent the behavior of these short-lived radioisotopes on the sediment bed. This paper describes the model and presents results from a set of idealized, one-dimensional (vertical) test cases. The model configuration represented fluvial deposition followed by periods of episodic storm resuspension. Sensitivity tests explored the influence on seabed radioisotope profiles by the intensities of bioturbation and wave resuspension and the thickness of fluvial deposits. The intensity of biodiffusion affected the persistence of fluvial event beds as evidenced by 7Be. Both resuspension and biodiffusion increased the modeled seabed inventory of 234Th. A thick fluvial deposit increased the seabed inventory of 7Be and 234Th but mixing over time greatly reduced the difference in inventory of 234Th in fluvial deposits of different thicknesses.en_US
dc.description.sponsorshipThe Bureau of Ocean Energy Management (BOEM) provided funding for Birchler, Harris, and Kniskern. During his M.S. program Birchler received additional funds from VIMS’ Office of Academic Studies. This work was partially supported by the U.S. Geological Survey, Coastal and Marine Geology Program.en_US
dc.publisherAmerican Meteorological Societyen_US
dc.relation.urihttps://doi.org/10.3390/jmse6040144
dc.rightsAttribution 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/*
dc.subjectnumerical modelen_US
dc.subjectsediment transporten_US
dc.subjectmarineen_US
dc.subjectshort-lived radioisotopesen_US
dc.titleSediment transport model including short-lived radioisotopes: Model description and idealized test casesen_US
dc.typeArticleen_US
dc.identifier.doi10.3390/jmse6040144


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Attribution 4.0 International
Except where otherwise noted, this item's license is described as Attribution 4.0 International