Chemical Composition of Water and Bottom Sediments in the Beysug Estuary of the Sea of Azov (Based on Field Studies, 2018)

A. D. Sazonov

Federal Research Center the Southern Scientific Centre of Russian Academy of Sciences, Rostov-on-Don, Russian Federation

e-mail: alexei.sazonow2016@ya.ru

Abstract

Purpose. The purpose of the study is to present the geochemical characteristics of the Beysug Estuary (the Sea of Azov) based on the data obtained during field studies of the chemical composition of water and bottom sediments in spring, summer and autumn of 2018.

Methods and Results. Water and bottom sediments were sampled in the western part of the estuary under calm weather conditions. The chemical composition of water was assessed using the following parameters: major ions (chlorides, sulfates, bicarbonates, magnesium, calcium, sodium, and potassium), nutrients (total nitrogen and its mineral forms, total phosphorus and phosphate phosphorus), petroleum products, organic matter, metal compounds (iron, copper, zinc, lead, cadmium, nickel, arsenic, chromium, mercury), phenols, benzo(a)pyrene, and synthetic surfactants. The grain-size composition of bottom sediments, as well as the mass fractions of sulfate ions, phosphate ions, petroleum products and phenols in the sediments, was determined. The obtained results indicate that, during the field research period, the ionic composition of the water in the studied area of the estuary (salinity ranged from 16.0 to 18.1) was stable. The concentrations of the studied forms of nitrogen and phosphorus exhibited pronounced seasonal variability (except for nitrite nitrogen). A similar trend was characteristic of petroleum products and organic matter. Slight exceedances of the maximum permissible concentrations were noted for readily oxidizable organic matter (BOD₅) (by 1.5–1.6 times), iron compounds (by 1.3–5.2 times), petroleum products (by 1.5–1.8 times) and ammonium ions (by 1.6 times). In most cases, trace element concentrations in water were below the detection limits of the applied analytical methods. The grain-size composition of bottom sediments showed a predominance (> 60%) of the aleurite-pelitic fraction (0.01–0.05 mm). The concentrations of petroleum products and phenols in the bottom sediments exhibited variability, while those of sulfate ions and phosphate ions remained relatively stable.

Conclusions. The geochemical parameters of water and bottom sediments in the Beysug Estuary are mainly determined by the prevailing hydrometeorological conditions, which govern the patterns of pollutant migration and accumulation.

Keywords

pollution, wetlands, chemical composition, heavy metals, nutrients, bottom sediments, eastern Azov region

Acknowledgements

The publication was prepared within the framework of the state assignment of the SSC of RAS (state registration No. 125012100503-4). Field observations were performed jointly with the staff of the Geoecology and Applied Geochemistry Department at Southern Federal University. The author is grateful to V.E. Zakrutkin, O.S. Reshetnyak, and E.V. Gibkov.

About the authors

Aleksey D. Sazonov, Junior Researcher, Laboratory of Hydrology and Hydrochemistry, Federal Research Center the Southern Scientific Centre of Russian Academy of Sciences (41 Chekhov Ave., Rostov-on-Don, 344006, Russian Federation), CSc. (Geogr.), ORCID ID: 0000-0002-1700-9314, ResearcherID: PHO-8323-2026, Scopus Author ID: 57871089700, SPIN-code: 4174-8079, alexei.sazonow2016@ya.ru

Original russian text

Original Russian Text © A. D. Sazonov, 2026, published in MORSKOY GIDROFIZICHESKIY ZHURNAL, Vol. 42, Iss. 4, pp. 601–610 (2026)

For citation

Sazonov, A.D., 2026. Chemical Composition of Water and Bottom Sediments in the Beysug Estuary of the Sea of Azov (Based on Field Studies, 2018). Physical Oceanography, 33(4), pp. 626-633.

References

  1. Matishov, G.G., ed., 2011. Ecological Atlas of the Sea of Azov. Rostov-on-Don: SSC RAS Publishers, 328 p. (in Russian).
  2. Grigorenko, K.S. and Matishov, G.G., 2025. Mineralization of Small Watercourses of the Eastern Cis-Azov Region in Modern Low-Water Conditions. Meteorologiya i Gidrologiya, (11), pp. 124-131. https://doi.org/10.52002/0130-2906-2025-11-124-131 (in Russian).
  3. Pogorelov, A.V., Lipilin, D.A. and Kuzyakina, M.V., 2024. On Technogenic Degradation of River Systems in the Eastern Azov Region: Hydrographic Aspect. Geology and Geophysics of Russian South, 14(3), pp. 243-259. https://doi.org/10.46698/i4469-5379-6925-p (in Russian).
  4. Krylenko, M., Kosyan, R. and Krylenko, V., 2016. Lagoons of the Smallest Russian Sea. In: R. Kosyan, ed., 2016. The Diversity of Russian Estuaries and Lagoons Exposed to Human Influence. Estuaries of the World. Cham: Springer International Publishing, pp. 111-148. https://doi.org/10.1007/978-3-319-43392-9_5
  5. Grechushkina, N.A., Demina, O.N., Sorokin, A.N. and Golub, V.B., 2011. Plant Communities of the Association Artemisio Santonicae-Elytrigietum Elongatae Dubyna, Neuhäuslová et Shelyag-Sosonko in Dubyna, Neuhäuslová 2000 (Class Scorzonero-Juncetea Gerardii Golub et al. 2001) in Yasenskaya Spit in the Azov Sea Coast of Russia. Izvestia of Samara Scientific Center of the Russian Academy of Sciences, 13(1), pp. 91-95 (in Russian).
  6. Denisenko, O.S., 2022. Determination of the Parameters of the Negative Impact on the Aquatic Bioresources of the Beisug Estuary of the Work on the Liquidation of Wells and the Flyover of the Field Gas Collection Point at the Beisug Gas Field. Scientific Review. Biological Sciences, (4), pp. 74-82. https://doi.org/10.17513/srbs.1297 (in Russian).
  7. Mohamed, Y.A., Bastiaanssen, W.G.M., Savenije, H.H.G., Van Den Hurk, B.J.J.M. and Finlayson, C.M., 2012. Wetland Versus Open Water Evaporation: An Analysis and Literature Review. Physics and Chemistry of the Earth, Parts A/B/C, 47–48, pp. 114-121. https://doi.org/10.1016/j.pce.2011.08.005
  8. Tong, Y., Feng, L., Wang, X., Pi, X., Xu, W. and Woolway, R.I., 2023. Global Lakes are Warming Slower than Surface Air Temperature due to Accelerated Evaporation. Nature Water, 1(11), pp. 929-940. https://doi.org/10.1038/s44221-023-00148-8
  9. Matishov, G.G., Grigorenko, K.S., Bulysheva, N.I. and Moskovets, A.Yu., 2021. New Data about the Function of Underground and Black Sea Waters in the Azov-Don Basin during the Lack of Water Period. Science in the South of Russia, 17(2), pp. 34-48. https://doi.org/10.7868/S25000640210204 (in Russian).
  10. Berdnikov, S.V., Dashkevich, L.V. and Kulygin, V.V., 2022. A New State in the Hydrological Regime of the Sea of Azov in the 21th Century. Doklady Earth Sciences, 503(1), pp. 123-128. https://doi.org/10.1134/S1028334X22030059
  11. Korablina, I.V., Pavlenko, L.F., Klimenko, T.L., Anokhina, N.S., Ekilik, V.S., Savchuk, I.A. and Ryzhkova, V.V., 2021. Characterization of Oil Pollution of the Azov Sea in 2016-2020. Aquatic Bioresources and Environment, 4(1), pp. 19-27. https://doi.org/10.47921/2619-1024_2021_4_1_19 (in Russian).
  12. Reshetnyak, O.S. and Zakrutkin, V.E., 2016. Bottom Sediments as a Source of Secondary Water Pollution by Metals (According to the Laboratory Experiment). Bulletin of Higher Educational Institutions. North Caucasus Region. Natural Sciences, (4), pp. 102-109. https://doi.org/10.18522/0321-3005-2016-4-102-109 (in Russian).
  13. Zhezherya, V.A., Zhezherya, T.P., Linnik, P.M. and Osipenko, V.P., 2023. Experimental Simulation of the Influence of Temperature on the Migration of Substances from Bottom Sediments. Hydrobiological Journal, 59(6), pp. 83-98. https://doi.org/10.1615/HydrobJ.v59.i6.70
  14. Gurov, K.I. and Fomin, V.V., 2021. Mathematical Modeling the Dynamics of the Bottom Sediments Granulometric Composition in the Balaklava Bay Affected by the Wind Waves. Physical Oceanography, 28(1), pp. 78-89. https://doi.org/10.22449/1573-160X-2021-1-78-89

Files

Full text

JATS XML