Abstrakti
The Finnish Archipelago Sea (AS) has long been subject to intensive anthropogenic phosphorus (P) loading. The area suffers from seasonal hypoxia and cyanobacterial blooms despite reductions in nutrient discharge from the catchment and point sources. Internal loading may even dominate the P budget. Previous estimates of internal P loading have limitations (e.g., in spatial coverage and infrequent measurements). We present the first area-wide estimates of the magnitude of internal P loading based on the long-term release of P stored in the sediments. Modelling the internal P loading in the AS is challenging due to the complexity of biogeochemical processes in the sediment-water interface, as well as the heterogenic topography of the seafloor. Instead, we calculated estimates of internal P loading based on data from previous studies on sequential chemical extraction of sediment P, sediment physical characteristics (e.g., organic content, location of muddy seabed substrates), and near-bottom oxygen (O2) conditions. The estimates in three scenarios of contrasting O2 conditions were based on potentially mobile P pools in the sediments, recycled from sediment to water (i.e., loosely-bound or exchangeable P, P bound to reducible iron oxy(hydr)oxides, and labile organic P). The potentially mobile P pools were determined by chemical extraction methods (modified from Psenner et al., 1984 and Ruttenberg, 1992). The internal P loading under presumable O2 conditions was estimated to be fivefold that of waterborne P input to the AS; comparable to previous estimates for hypoxic areas in the Baltic Sea. Our estimates revealed wide spatial variability in the internal P loading, depending on O2 conditions and seabed sediment substrate. The site-specific P release estimates are included in a water quality model used by regional authorities, which increases the model's reliability for estimating the impact of human activities on the water quality across the AS.
| Alkuperäiskieli | Englanti |
|---|---|
| Artikkeli | 173717 |
| Julkaisu | Science of the Total Environment |
| Vuosikerta | 942 |
| DOI - pysyväislinkit | |
| Tila | Julkaistu - 10 syysk. 2024 |
| OKM-julkaisutyyppi | A1 Julkaistu artikkeli, soviteltu |
Rahoitus
The model development was funded by the Ministry of the Environment of Finland , the Finnish Environment Institute , the Finnish Meteorological Institute and the Centres for Economic Development, Transport and the Environment . We want to thank the project SEABED in the EU Central Baltic INTERREG IVA programme for sediment and water data and the PyWQM model code, and the government of \u00C5land for the water quality monitoring data in \u00C5land. The bathymetric data used to compile the coastal grid for the hydrodynamic model was obtained from the Finnish Transport Agency's coastal nautical charts and the contemporaneous VELMU map service (no longer available). Salinity and temperature profiles for the open sea boundary at Kattegat were produced using E.U. Copernicus Marine Service Information ( http://marine.copernicus.eu/ ). Sea level data was obtained from the SMHI open data service ( http://opendata-download-ocobs.smhi.se/explore/ ), licensed under the Creative Commons CC-BY-2.5 license. STR\u00C5NG data used here are from the Swedish Meteorological and Hydrological Institute (SMHI) and were produced with support from the Swedish Radiation Protection Authority and the Swedish Environmental Agency. Life IP Biodiversea project provided facilities for the manuscript preparation. We thank Dr. Johanna Mattila for her valuable comments on improving the manuscript and Dr. Roxana Preston for linguistic proofreading.
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