Polycyclic aromatic hydrocarbon (PAH) source, sediment deposition patterns, and particle geochemistry as factors influencing PAH distribution coefficients in sediments of the Elizabeth River, VA, USA

Citation
S. Mitra et al., Polycyclic aromatic hydrocarbon (PAH) source, sediment deposition patterns, and particle geochemistry as factors influencing PAH distribution coefficients in sediments of the Elizabeth River, VA, USA, MAR CHEM, 66(1-2), 1999, pp. 113-127
Citations number
43
Categorie Soggetti
Aquatic Sciences","Earth Sciences
Journal title
MARINE CHEMISTRY
ISSN journal
03044203 → ACNP
Volume
66
Issue
1-2
Year of publication
1999
Pages
113 - 127
Database
ISI
SICI code
0304-4203(199907)66:1-2<113:PAH(SS>2.0.ZU;2-Q
Abstract
Sediments and pore waters from two sites in the urbanized Elizabeth River, Virginia were sampled for levels of polycyclic aromatic hydrocarbons (PAHs) . Pore water PAH concentrations were similar between Sites 1 and 2, despite sediment PAH concentrations being much greater at Site 2. Organic carbon-n ormalized distribution coefficients (K-OC)(obs) for all PAHs were significa ntly higher at Site 2 compared to Site 1, but varied similar to 2-3 orders of magnitude between the top and bottom of the core in the sediments at Sit e 1. PAH distribution between sediments and pore waters at Site 1 were most notably related to the bimodal sediment deposition patterns as depicted by X-radiograph depth profiles, and PAH isomer concentration ratios. Sediment ary organic carbon/nitrogen ratios, lignin-phenol concentrations, soot carb on, and particle surface area both before and after organic digestion, were also analyzed in order to assess the role of sediment geochemistry on PAH (K-OC)(obs). Different factors were determined to control particle surface area at each site, offering insight into explaining observed PAH distributi on coefficients. At Site 1, sediment organic matter was inaccessible for di gestion and perhaps PAH partitioning as well. Sorption of PAHs to mineral s urfaces explains low values for PAH distribution coefficients observed in t he deeper sediments in this core. At Site 2, large and invariant (K-OC)(obs ) may result from sediments comprised of particles (e.g., woody debris) inf used with creosote and coated with organic matter sequestering PAHs within the particle matrix. Our results indicate there is significant heterogeneit y in PAH distribution coefficients in estuarine sediments, which may be att ributed to sediment deposition patterns, PAH source(s), and sediment geoche mistry. (C) 1999 Elsevier Science B.V. All rights reserved.