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Distribution and transport of particle-bound polycyclic aromatic hydrocarbons in a river-influenced continental margin; the northern Gulf of Mexico
Conference proceeding

Distribution and transport of particle-bound polycyclic aromatic hydrocarbons in a river-influenced continental margin; the northern Gulf of Mexico

Puspa L Adhikari, Kanchan Maiti and Anonymous
American Geophysical Union Fall Meeting, Vol.2017
American Geophysical Union 2017 fall meeting
12-2017

Abstract

Geochemistry of rocks, soils, and sediments
Polycyclic aromatic hydrocarbons (PAHs) are particle-reactive and get preferentially sorbed on particulate organic carbon (POC), thus, the transport and fate of POC in aquatic systems plays an important role in biogeochemical cycling of PAHs. In this study, we examine POC and PAHs in finer suspended particulate matter collected from the Louisiana coast, shelf and slope--progressively south-west transect along the direction of the Mississippi River plume, and also from a transect of Atchafalaya River. The concentrations of total particulate PAHs (Sigma PAH43) varied between 0.92 to 7.04 ng/L, while POC varied between 4 to 131 mu g/L. The concentrations of total particulate Sigma PAH43 as well as individual PAH analytes were significantly positively correlated to the concentrations of POC which indicates that the concentrations and transport of POC plays an important role in distribution of PAHs in marine systems. The river influence, characterized by the change in salinity, had significant negative correlation with both the concentrations of particulate PAHs and POC. These results show that the Mississippi River derived particle influx can be an important vector in delivering particle-reactive hydrophobic organic pollutants such as PAHs into the river dominated continental ecosystems in the northern Gulf of Mexico. The underlying seafloor sediment PAHs' concentration and accumulation rates were not correlated to the water column particulate PAH and POC concentrations, which is attributed to re-mineralization during vertical transport, sediment resuspension/redistribution and different timescales of comparison.

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