Abstract

The following three passages and the respective references were not included in the published version. They should have been added to the paragraphs specified below. 4 studied the effects of different land management practices on deep seepage and solute leaching based on soil water content and tension time series measured in 3 m soil depth. The field experiment was designed to study the effects of land use and land management on deep seepage and solute leaching (3; 1). Time series of soil moisture and soil water tension were continually measured in high temporal solution, and soil water samples were taken in different soil depths down to 3 m. The measurements started in 1994 and continue today. Our findings about the small functional heterogeneity at the experimental site confirmed the basic assumption by 2 that relative soil moisture dynamics at different positions in the deep vadose zone are very similar. They developed and tested a field method for quantifying deep seepage and solute leaching based on tension and water content measurements and applied it successfully at 40 plots in northeast Germany (3; 4).

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