Sediment Dissolved Organic Carbon Release in the Baltic Sea

Dissolved organic carbon (DOC) flux evaluated by Fick's first law of diffusion. The values were evaluated using the pore water dissolved organic matter, average weighted apparent molecular weight of DOM measured in samples collected by Rhizon samplers from the water 2 cm above the sediment and the top 10 cm of the sediment cores at 2 cm intervals. The porosity was evaluated as sediment water content was obtained from sediment samples collected via slicing of the upper 10 cm of sediment cores over 2 cm intervals. The sediment cores were recovered using GeMax sediment corer. These samples were collected between 2020 and 2021 during cruises onboard RV Oceania (Institute of Oceanology of the Polish Academy of Sciences), which took place in spring, autumn, and winter, to the Central and Southern Baltic Sea, i.e., Eastern Gotland Basin, Bornholm Basin, and Gdansk Basin. The reported DOC sediment fluxes are the final product.

Data and Resources

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Cite this as

Loginova, Alexandra, Kowalczuk, Piotr (2024). Dataset: Sediment Dissolved Organic Carbon Release in the Baltic Sea. https://doi.org/10.1594/PANGAEA.967081

DOI retrieved: 2024

Additional Info

Field Value
Imported on November 30, 2024
Last update November 30, 2024
License CC-BY-4.0
Source https://doi.org/10.1594/PANGAEA.967081
Author Loginova, Alexandra
Given Name Alexandra
Family Name Loginova
More Authors
Kowalczuk, Piotr
Source Creation 2024
Publication Year 2024
Resource Type text/tab-separated-values - filename: Loginova_DOC_flux
Subject Areas
Name: Ecology

Related Identifiers
Title: Qualitative variability of dissolved organic matter in the Baltic Sea sediments apparent from fluxes and optical properties
Identifier: https://doi.org/10.3389/fmars.2024.1433199
Type: DOI
Relation: References
Year: 2024
Source: Frontiers in Marine Science
Authors: Loginova Alexandra N , Wünsch Urban J , Zabłocka Monika , Cherkasheva Aleksandra , Szymczycha Beata , Kuliński Karol , Winogradow Aleksandra , Kowalczuk Piotr .