66 Marine/Coastal Science I: Salt Marshes and Coastal Deposits

Monday, 5 November 2012
8:00 AM - 12:00 PM
218AB

SEDIMENT DYNAMICS OF THE ALBEMARLE-PAMLICO ESTUARINE SYSTEM, NORTH CAROLINA

Paper number: 66-7
Program: Technical Sessions
Time: 9:30 AM – 9:45 AM

Authors

  • D. Reide Corbett Presenting Author
    East Carolina University & UNC Coastal Studies Institute, Greenville, NC
  • J.P. Walsh
    East Carolina University & UNC Coastal Studies Institute, Greenville, NC
  • Devon Eulie
    East Carolina University, Greenville, NC

Abstract

Estuaries are critical habitats as well as places where people live, recreate, and make their livelihood. Additionally, they are sites where land and sea interact, and sediments, and associated pollutants and carbon, are deposited, remobilized and accumulated. Many processes, such as river discharge, waves, tides, and sea-level rise, are operating in estuaries to cause sediment dynamics, impacting humans and organisms as a result. Recent research we have been engaged in across the Albemarle-Pamlico Estuarine System (APES) has investigated the sediments dynamics of this important estuary.

The APES is the second largest estuary in the continental United States, consisting of the Albemarle and Pamlico sounds and the Pamlico River and Neuse River sub-estuaries. Although expansive in size, the system is shallow with minimal tidal range. Water and sediment discharge into the APES is modest, and the existence of few inlets along the Outer Banks limits mixing with the Atlantic Ocean. Human impact on the drainage basin and estuarine system is moderate and increasing over time.

Over the last five years, a considerable volume of sedimentary process data has been collected over various timescales and locations in the APES. More specifically, work has included: deployments of instrumented tripods to examine seabed dynamics; collection and analysis of shallow cores and GIS investigation of aerial photographs and other data. This wealth of data highlights several insights: 1) significant storage of sediment in the fluvial floodplain, 2) seabed erosion and deposition is inconsistent, but net accumulation of 2-4 mm/y is widespread; and 3) shoreline change although variable is generally eroding (~0.25 m/y), supplying much sediment; 4) storm waves and river floods are controls on this large but shallow estuarine system.