Summary
In connection with hydrographical investigations in a high mountain lake the ice was also analysed. These analyses indicated relatively high content of nutrients (PO4, NO3 + NO2, and NH4) in the ice, and the most surprising feature was the content of PO4 and its irregular, vertical as well as horizontal, distribution.
Freezing experiments in the laboratory showed that waters from the lake increased in PO4 content after completely freezing in a sample bottle. These experiments indicate that PO4 can be released from some organic substances during the freezing process, and that this phenomenon also applies to the ice frozen on the lake.
On the basis of hydrographical research just after the spring thaw, the relatively great amount of PO4 in the ice of the lake (and probably also in the ice of the drainage area) seems to have a great influence on the PO4 content of the water masses.