Germanium-68 as a tracer for silicon fluxes in freshwater sediment.

The sorption of Si may decisively influence the P dynamics in surface sediment through competitive ligand exchange mechanisms. Many aspects of the process, such as the impact of Si dissolving from diatoms, are both insufficiently known and difficult to monitor by quantitative analyses due to the ubiquitousness of Si in sediment. Since the radioactive isotopes of Si have impractical half-times, the applicability of 68Ge as a tracer for Si additions in both inorganic and biogenic form to freshwater sediment (Lake Vesijärvi, Southern Finland) was studied in a 24-h laboratory experiment. The 68Ge-label was added to the sediment with either inorganic Si (940mg l(-1)) or diatoms (3.2 x 10(6) cellsl(-1)), and the distributions of the 68Ge-label and the different forms of added Si between the interstitial water and sequentially extracted, solid-phase sediment pools were critically examined. The inorganic Si addition significantly increased the amount of Si in the interstitial water and in the reversibly bound fraction, while the diatom addition had no discernible effects. The relative distribution of Si and 68Ge between the various sediment pools indicated that the first sorption phase of the added inorganic Si was similar to that reported for P. The high concentration of diatom-derived 68Ge-labelled Si in the interstitial water and in the easily soluble, reversibly bound pool indicated rapid dissolution of the added diatoms. The comparable distributions of the diatom-derived and inorganic Si-derived 68Ge-label within the studied pools indicated that the sorption of Si dissolving from diatoms in surface sediment closely resembles that of an inorganic addition of Si. Caution about the chemical speciation of the 68Ge-label is, however, advisable in sediment environments. Fractionation procedures designed for e.g. P may also be of limited use when applied to a different element, such as Si.