Influence of water level fluctuation on the spatial dynamic of the water chemistry at Lake Ferto/Neusiedler See

Lake Ferto/Neusiedler See is a steppe lake Situated on the Hungarian-Austrian border with a surface area of 309 km(2). It is an extremely shallow take with regulated outflow. 54% of the whole lake and 85% of the Hungarian part (75 km(2)) is covered by reed. There are numerous reedless areas (inner ponds) of variable size within the reed belt, which is enmeshed with canals connecting the inner ponds with the open water areas. Fundamental differences were recorded in the water chemistry of the three water type areas, open water, canals and inner ponds. The degree of these differences is basically determined by the distance from the open water areas and the water level of the actual years. An extremely high, an average and an extremely low water level year was examined, in order to present the spatial and temporal differences in the water chemistry of the investigated water bodies. Differences due to the water level fluctuation between years in the three different water types are discussed on the basis of electrical conductivity, cation, and anion concentration changes of the water. Our results support the concept of high instability of Lake Ferto and describe habitats with remarkable temporal and spatial variability. The high influence of water level on habitat conditions at different sites of the lake recommend a carefull water level regulation strategy.