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Characteristics of bottom sediments in the Kievka Bay of the Japan Sea

https://doi.org/10.26428/1606-9919-2024-204-905-916

EDN: WHQUNV

Abstract

Basic properties of bottom sediments, including organic carbon content, are determined to understand biogeochemical cycles in the marine environment. The samples were collected using a geological column sampler from the upper 10-centimeter layer of the sediments at the depth of 12.2–99.0 m in Kievka Bay in the 83rd cruise of RV Academician M.A. Lavrentiev. The bottom sediments in Kievka Bay are distinguished by significant content of organic carbon, in the medium to high categories, and high levels of major nutrients in the organic fraction, such as nitrogen, phosphorus and potassium. Their particle-size composition corresponds mainly to sandy loams, with prevalence of silicon, aluminum and iron in the mineral skeleton that is similar to coastal soils. The content of organic carbon and total nitrogen in the bottom sediments of Kievka Bay correlates positively with the portion of physical clay fraction. The same analytical techniques used for both bottom sediments and coastal soils allow to consider the continental-ocean transition zone as a single system.

About the Authors

O. V. Nesterova
Far Eastern Federal University
Russian Federation

Olga V. Nesterova, Ph.D., assistant professor

10, Ajax Bay, Russky Island, Vladivostok, 690922



A. V. Brikmans
Far Eastern Federal University
Russian Federation

Anastasia V. Brikmans, Ph.D, assistant professor

10, Ajax Bay, Russky Island, Vladivostok, 690922



V. G. Tregubova
Far Eastern Federal University
Russian Federation

Valentina G. Tregubova, Ph.D, assistant professor

10, Ajax Bay, Russky Island, Vladivostok, 690922



A. M. Gilyov
Far Eastern Federal University
Russian Federation

Andrey M. Gilyov, master

10, Ajax Bay, Russky Island, Vladivostok, 690922



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For citations:


Nesterova O.V., Brikmans A.V., Tregubova V.G., Gilyov A.M. Characteristics of bottom sediments in the Kievka Bay of the Japan Sea. Izvestiya TINRO. 2024;204(4):905-916. (In Russ.) https://doi.org/10.26428/1606-9919-2024-204-905-916. EDN: WHQUNV

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ISSN 1606-9919 (Print)
ISSN 2658-5510 (Online)