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Atmospheric Deposition of Acidifying and Eutrophicating Substances in Dune Slacks

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Abstract

The atmospheric input of nitrogen and potantial acid, and the composition of the leachate from the topsoil layer are quantified for eight dune slack sites differing in plant composition, on the Frisian islands of Terschelling and Schiermonnikoog. Basiphilous mesotrophic communities with many rare plant species grow in one site on Terschelling and two sites on Schiermonnikoog. Samples were taken in the period mid May 1992 – mid May 1993. Bulk atmospheric nitrogen deposition measured in an open collector was between 15–20 kg ha−1 yr−1 for the eight sites. On Terschelling, the deposition was slightly higher than on Schiermonnikoog. Ammonium was a third of the total amount of nitrogen deposited on Terschelling and half the amount of nitrogen deposited on Schiermonnikoog. The deposition of potential acid varied from 490 to 810 mol ha−1 yr−1. On Terschelling, the amount of potential acid was highest and around 800 mol ha−1 yr−1 for both sites. On Schiermonnikoog, the amount of potential acid was lowest for the dune slacks in the north-western part of the island and it showed an increase for slacks towards the eastern part of the island. Calcium is the main cation leached from the topsoil followed by sodium, magnesium and potassium. Nitrogen or ammonium hardly leached from the topsoil layer. The shift from basiphilous pioneer communities toward older and more acid stages of dune slack succession appears to be caused primarily by leaching of base cations rather than eutrophication.

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Sival, F.P., Strijkstra-Kalk, M. Atmospheric Deposition of Acidifying and Eutrophicating Substances in Dune Slacks. Water, Air, & Soil Pollution 116, 461–477 (1999). https://doi.org/10.1023/A:1005172221338

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