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• W2132317246 abstract "The Cape Fear River (CFR) is a low discharge river, which drains the largest areaof any rivers fully contained within North Carolina. The river is formed in the Piedmontby the convergence of the Haw and Deep Rivers and then flows southeast through thestate terminating into Long Bay in the Atlantic Ocean.Long Bay is the most southern in a series of bays along the North Carolina coast.mud drapes observed in the bottom sediment deposits of Long Bay are unique in that nosuch deposits are found in Onslow Bay to the North. The CFR is the most reasonablesource of this material, though no relationship has been shown between discharge fromthe river and variations in sediment composition and texture. The nature of these muds(permanent or mobile) is important as mud particles can provide a substrate by whichpollutants can be transported into the coastal ocean. If these deposits, then, are stablethey could serve as a sink for these pollutants while if they are mobile they may act tocontinually reintroduce these materials into the water column. Bi-monthly sampling ofboth TSS concentrations in the water column and surficial bottom sediment deposits atseven sites (site 1, site 2, site 5, site 6, site 7, site 8 and site 9), starting in the mouth of theriver and moving southwest away from the river mouth, occurred from September 2003through November 2004. Physical parameters like discharge, precipitation and windwere obtained from outside data sets collected by NOAA, the USGS, the Coastal OceanResearch and Monitoring Program, and the State Climate Office of North Carolina.Results show that when compared to the control site (site 1) located directly in themouth of the river, mean TSS concentrations at those two sites located closest to the CapeFear River mouth (sites 2 and 6) were significantly correlated. The organic content of bottom sediments at sites 2 and 6 was significantly and positively correlated to mudcontent of bottom sediments. In addition bottom sediment mud and organic content wassignificantly and positively correlated to three TSS concentration parameters. It wouldappear then that at least for those sites proximal to the river mouth a definitiverelationship between the TSS concentrations and bottom sediment deposits becomesmore clear.Those sites more distal from the mouth showed little if any variation in both TSSconcentrations and sediment composition except in rare occasions specifically followingpeak discharge events related to an extratropical storms. The infrequency of the samplingmade characterization of these more distal four site (site 5, site 7, site 8, and site 9)difficult, though with an increased frequency it may become possible to define the natureof variability seen at these locations. Site 7 especially would be expected to be defined asa site impacted by the river derived materials." @default.
• W2132317246 created "2016-06-24" @default.
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• W2132317246 date "2009-01-01" @default.
• W2132317246 modified "2023-09-22" @default.
• W2132317246 title "The influence of the Cape Fear River on characteristics of shelf sediments in Long Bay, North Carolina" @default.
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