Abstract

BackgroundThere are various ways for nutrients to enter aquatic ecosystems causing eutrophication. Phosphorus deposition through precipitation can be one pathway, besides point sources, like rivers, and diffuse runoff from land. It is also important to evaluate recent trends and seasonal distribution patterns of phosphorus deposition, as important diffuse source. Therefore, a long-term dataset was analysed including 23 years of daily phosphate bulk depositional rates and 4.5 years of total phosphorus (TP) bulk depositional rates. The study area was at the coastline of the southern Baltic Sea, an area which shows severe eutrophication problems.ResultsThe median daily deposition of phosphate was 56 µg m−2 day−1 (1.8 µmol m−2 day−1) at 4222 rain events. The median annual sum of phosphate deposition was 16.7 kg km−2 a−1, which is comparable to other European areas. The annual TP deposition depended strongly on methodological aspects, especially the sample volume. The median TP-depositional rates ranged between 19 and 70 kg km−2 a−1 depending on the calculated compensation for missing values, as not every rain event could be measured for TP. The highest TP-depositional rates were measured during summer (e.g. up to 9 kg TP km−2 in August 2016). There was no trend detectable for phosphate- and TP-depositional rates over the sampled period.ConclusionsDeposition of P is a considerable nutrient flux for coastal waterbodies. Median total annual deposition contributed 3 t (phosphate) to 10 t (TP) per year into the adjacent lagoon system, being therefore close to annual riverine inflows of 10 t phosphate and 20 t TP per year. However, the impact of precipitation is predicted to be higher in lagoon parts with fewer point sources for phosphorus, if equally distributed over the area of interest.

Highlights

  • There are various ways for nutrients to enter aquatic ecosystems causing eutrophication

  • We report P-depositional rates over 23 years of continuous rain water sampling and chemical analysis at the Biological Station Zingst (University of Rostock) at the southern Baltic Sea coast

  • Data evaluation and statistics Numerous precipitations events led to low volume samples which could not be analysed and ­PO4-P values are missing

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Summary

Introduction

There are various ways for nutrients to enter aquatic ecosystems causing eutrophication. The Baltic Sea is one of the largest brackish, non-tidal inland seas of the Northern Atlantic. It occupies a basin formed by glacial erosion during the last ice age about 13,000 years ago. In the early 1990s, the total annual nitrogen load to the Baltic Sea comprised 1.4 million t of which 69% were waterborne discharges (rivers, point and non-point sources), 10% were caused by ­N2 fixation through cyanobacterial blooms, while the rest, 21%, was atmospheric deposition onto the sea surface [6]. The remaining 31% of the P input to the Baltic Sea are not explicitly described [8] Other sources, such as atmospheric deposition, must be considered in more detail [9]

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