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Tammeorg, Olga; Nürnberg, Gertrud K.; Tõnno, Ilmar; Kisand, Anu; Tuvikene, Lea; Nõges, Tiina; Nõges, Peeter
Science of the total environment, 07/2022, Letnik: 829Journal Article
Sediment phosphorus (P) recycling is one of the key issues in lake water quality management. We studied sediment P mobility in Võrtsjärv, a large shallow lake in Estonia using both sorption experiments and long-term (1985–2020) monitoring data of the lake. Over the years studied, the lake has undergone a decline in external phosphorus loading (EL), while no improvement in phytoplankton indicators was observed. The results of the sorption experiments revealed that it may be successfully used as a tool to determine P forms involved in P retention, as up to 100% of the P from the water column was detected in sediments. Incubation of wet sediment is preferred to dry because of the sensitivity of organic P to desiccation. In the sediments of Võrtsjärv, the labile P (Lab-P) and iron bound (Fe-P) fractions are the major forms of the mobile pool that supply internal P load as sediment released P. The internal P load calculated from summer total P (TP) increases (ILin situ) in the water column was on average 42%, but could reach 240% of EL at extreme environmental conditions. ILin situ was correlated with the active area, which resembles the area involved in redox-related P release in polymictic lakes, and with the mean bottom shear stress in summer. ILin situ showed a similar decreasing pattern as the external P load over the years 1985–2020, and was likely driven by the decrease of the pool of releasable P. Similarly, the decreases in sediment loading by P retention in our P sorption experiment were associated with decreases in the concentration of the potentially mobile P forms (mainly Lab-P and Fe-P). These results show that changes in external P loading can successfully control internal P loading and are useful in water quality management of large lakes. Display omitted •We studied sediment P dynamics by sorption experiments and long-term data analysis.•Adsorption of P from water column was fully reflected in changes of sediment P fractions.•The labile P and Fe-P fractions were the major forms involved in P adsorption.•Internal P load decreased over the years 1985–2020, similar to external P load.•Changes in internal P load were driven by decrease in the pool of mobile P.
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