| HYDROGEOCHEMICAL PROCESSES IN LIMNIC SYSTEMS Introduction
Willersinnweiher
is an excavator lake in the highly industrialized area of Ludwigshafen/Rhein,
Germany. The pond is freequently used as recreation area for
the urban population for its water chemistry has to keep standards
of the European Community. The entry of nutrients from adjacent
agricultural areas and pollution by industrial and private sewage
in the last few decades led to an increasing eutrophication
of the lake which required complex efforts to improve its water
chemistry (Sandler
2000).
These days, the water quality of Willersinnweiher has improved
considerably. It exists a large data set on the lake's water
chemistry and physical construction and in the surrounding area
12 piezometers for the examination of surface water/groundwater
coupling were installed.
At Willersinnweiher
processes will be studied in different compartments of the dimictic
system: in the layered water column during stagnation in summer,
at the free water / pore water interface during the circulation
period and in the Quaternary shallow aquifer during the whole
year. Additionally, sediment cores and material from sediment
traps as well as particles from the water column will be investigated.

Projects
Former
Projects
Associated
works at Willersinnweiher
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