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Assessment of modern sediment storage in the floodplain of the lower Tar River, North Carolina / by Dimitri Quafisi.

Author/creator Quafisi, Dimitri
Other author/creatorWalsh, J. P. (John Patrick), 1973- degree supervisor.
Other author/creatorCorbett, D. Reide (David Reide), 1971- degree supervisor.
Other author/creatorEast Carolina University. Department of Geological Sciences.
Format Theses and dissertations, Electronic, and Book
Publication Info[Greenville, N.C.] : East Carolina University, 2010.
Description110 pages : illustrations (some color), maps (some color), digital, PDF file
Supplemental Content Access via ScholarShip
Subject(s)
Summary Rivers transport water, sediment, and other constituents from the continent to the sea, but in route material can often become stored temporarily or permanently. Along the Atlantic Coast of the United States, coastal plain rivers such as the Tar River are characterized as low-gradient meandering systems that develop wide floodplains which are subjected to frequent and prolonged flooding. As a result, these rivers are believed to experience storage of sediment, particularly near their estuarine mouths. The lower portion of rivers and their attached estuaries are also environmentally and economically important serving as critical habitat (e.g., nurseries for fish), recreational areas, and transportation pathways. Excess sediment is often considered a significant pollutant and can have adverse effects on biota. Suspended sediment also can supply excess nutrients and trace metals from anthropogenic activity. Previous work in North Carolina suggests that alluvial storage can make up the majority (>50%) of the total sediment delivered to rivers. This study more closely examines the nature of lower floodplain sediment storage and more specifically focuses on calculating sediment accumulation along the Tar River. Cores were collected from three sites along seven different transects perpendicular to the main channel. Analysis of ²¹⁰Pb and ¹³⁷Cs were employed to calculate sediment accumulation rates, and grain-size data were made to inform radionuclide and sedimentation interpretations. Sedimentation rates within the study area range from 0.09 to 1.08 cm/yr. However, several sites appear to have non-steady-state deposition possibly due to major overbank flood events. Grain-size data indicate a mixture of sand and mud at all sites with some variability in the nature of sediment accumulating. Using core observations and LiDAR topographic data, storage across the system is estimated to be approximately 1.26 x 10⁵ t/yr or roughly 66% of the total incoming sediment measured at Tarboro, NC (1.89 x 10⁵ t/yr) in previous works.
General notePresented to the faculty of the Department of Geological Sciences.
General noteAdvisors: John Walsh and D. Reide Corbett.
General noteTitle from PDF t.p. (viewed April 13, 2011).
Dissertation noteM.S. East Carolina University 2010.
Bibliography noteIncludes bibliographical references.
Technical detailsSystem requirements: Adobe Reader.
Technical detailsMode of access: World Wide Web.

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