Loamy soils have a high buffering and filtration function with low water permeability and a high effective cation exchange capacity. These requirements are met primarily by the soils on the Teltow and Barnim boulder marl plateaus. The sandy soils of the glacial valley only have a low ability to filter and buffer pollutants.
01.12.3 Buffering and Filtration Function
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01.12.3 Buffering and Filtration Function
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