Presence of aliphatic and polycyclic aromatic hydrocarbons in near-surface sediments of an oil spill area in Bohai Sea.

Mar Pollut Bull

Key Laboratory of Petroleum Resources, Gansu Province/Key Laboratory of Petroleum Resources Research, Institute of Geology and Geophysics, Chinese Academy of Sciences, Lanzhou, Gansu 730000, People's Republic of China.

Published: November 2015

AI Article Synopsis

  • The study analyzed 50 sediment samples from an oil spill site in the Bohai Sea to identify sources of organic matter and oil components.
  • The concentrations of specific n-alkanes and PAHs were measured, showing ranges of 0.88-3.48μg g(-1) for C15-35 n-alkanes and 9.97-490.13ng/g for priority pollutant PAHs.
  • Findings indicated that terrestrial organic matter came from river-transported higher plants, while marine organic matter was linked to plankton and aquatic plants, with evidence of crude oil infiltrating from geological faults.

Article Abstract

In order to determine the source of organic matter and the fingerprint of the oil components, 50 samples collected from the near-surface sediments of the oil spill area in Bohai Sea, China, were analyzed for grain size, total organic carbon, aliphatic hydrocarbons (AHs), and polycyclic aromatic hydrocarbons (PAHs). The concentrations of C15-35 n-alkanes and 16 United States Environmental Protection Agency (US EPA) priority pollutant PAHs were found in the ranges of 0.88-3.48μg g(-1) and 9.97-490.13ng/g, respectively. The terrestrial organic matters characterized by C27-C35 n-alkanes and PAHs, resulting from the combustion of higher plants, are dominantly contributed from the transportation of these plants by rivers. Marine organic matters produced from plankton and aquatic plants were represented by C17-C26 n-alkanes in AHs. Crude oil, characterized by C17-C21 n-alkanes, unresolved complex mixture (UCM) with a mean response factor of C19 n-alkanes, low levels of perylene, and a high InP/(InP+BghiP) ratio, seeped into the oceans from deep hydrocarbon reservoirs, as a result of geological faults.

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Source
http://dx.doi.org/10.1016/j.marpolbul.2015.09.009DOI Listing

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