As reported from marine systems, we found that also in 15 prealpine la
kes N2O concentrations were strongly correlated with O-2 concentration
s. In oxic waters below the mixed surface layer, N2O concentrations us
ually increased with decreasing O-2 concentrations. N2O is produced in
oxic epilimnia, in oxic hypolimnia and at oxic-anoxic boundaries, eit
her in the water or at the sediment-water interface. It is consumed, h
owever, in completely anoxic layers. Anoxic water layers were therefor
e N2O undersaturated. All studied lakes were sources for atmospheric N
2O, including those with anoxic, N2O undersaturated hypolimnia. Howeve
r, compared to agriculture, lakes seem not to contribute significantly
to atmospheric N2O emissions.