When oxygen is present in the bottom water phosphorus is buried in the bottom sediments, and the amount of phosphorus available for e.g. cyanobacteria diminishes.
When oxygen is lacking phosphorus is released back to the water column – a situation that we would like to avoid and therefore also to better understand.
The study “Benthic Pelagic Coupling in the Baltic Sea: the effect of redox changes on sediment P release and implications for water quality” improved our knowledge of the mechanisms affecting the burial of phosphorus in the Baltic Sea.
Caroline Slomp, University of Utrecht
2011-01-01 - Final report - scientific article
Sedimentary phosphorus dynamics and the evolution of bottom-water hypoxia: A coupled benthic–pelagic model of a coastal system
2009-11-16 - Popular report
Phosphorus dynamics in Baltic Sea sediments 2007-2009