Hydrocarbon pollution in the waters and sediments of the Kerch Strait

The results of studying the content and composition of aliphatic hydrocarbons and polycyclic aromatic hydro-carbons in the suspended particulate matter of surface waters and in the surface layer of bottom sediments in 2019-2021 in the Kerch Strait in comparison with earlier studies in other areas of the Black Sea (Theodosia Gulf, Tuapse area, Coastal waters of the Crimean Peninsula, Big Sochi, Central part of the Sea) are presented. Despite the high concentrations of aliphatic hydrocarbons (especially in the waters of the strait itself: 28-254 on average 87 mu g/L. The highest content of aliphatic hydrocarbons was confined to the cross-section through the Kerch Strait. Accumulation of aliphatic hydrocarbons, as well as the suspended particulate matter, occurs in the western part of the Strait, which is associated with the predominant wind direction and coastal orography. The composition of alkanes did not correspond to the smooth distribution of homologues characteristic of oil. Their distribution was bimodal in most samples, which may indicate a mixed genesis of alkanes. Among the low- molecular-weight alkanes either even numbered autochthonous alkanes n-C16, -C18, -C22, arising during the microbial transformation of aliphatic hydrocarbons, or n-C17, indicating the inclusion of phyto- and zooplankton alkanes, prevailed. Despite the different sources of hydrocarbons input, the distribution of the total concentra-tions of aliphatic hydrocarbons and polycyclic aromatic hydrocarbons basically coincided. Polycyclic aromatic hydrocarbons composition was dominated by fluoranthene and pyrene, which are formed in high-temperature combustion processes Low values of the Sigma naphthalenes/Phen ratio (0.05-0.11) may indicate an insignificant inclusion of petroleum polyarenes. In contrast to suspension of surface waters, the highest content of hydrocarbons in the surface sediments was found not in the strait, but at stations in areas with aleurite-pelitic sediments, which is due to the pattern of currents in these areas and the higher sorption capacity of finely dispersed sediments. The average Corg content in July 2020, was 1.8 times lower (0.34%) than in September 2019 (0.63%), and aliphatic hydrocarbons, on the contrary, was 2.2 times higher (47 mu g/g) than in April 2019 (21 mu g/g). In surface sediments the maximum concentration of aliphatic hydrocarbons was established in July 2020 (233 mu g/g), and the highest average content in July 2021 (58 mu g/g). This area is also associated with higher concentrations of aliphatic hydrocarbons in the composition of Corg ->= 1%. The composition of alkanes in surface sediments differed from their compo-sition in suspension. The ratio of low-to-high molecular weight homologues (L/H =0.08-0.54) was lower and the odd-to-even ratio (CPI =1.19-4.58) was higher than in particulate matter. Due to the coarse composition of sediments, the content of polycyclic aromatic hydrocarbons in their surface layer was lower (0-631 ng/g) compared to other areas of the Black Sea. In their composition, along with fluoranthene and pyrene, methylated naphthalene homologues also belonged to the dominant compounds. Correlation analysis of individual poly-arenes, as well as factor analysis, indicates their mixed genesis oil +pyrogenic, with the preference of the latter in most samples. The entry of pollutants into the marine environment increases the hydrocarbons content in water and bottom sediments, creating a modern hydrocarbon background.

Automated summary

The study investigates the content and composition of aliphatic hydrocarbons and polycyclic aromatic hydrocarbons in the suspended particulate matter and surface layer of bottom sediments in the Kerch Strait. The findings indicate higher concentrations of aliphatic hydrocarbons in the western part of the strait and lower concentrations of polycyclic aromatic hydrocarbons in the surface sediments. The study also highlights the increase in hydrocarbon content in water and sediments due to pollutant entry into the marine environment.