BOKU University, Institute of Soil Physics and Rural Water Management, Department of Landscape, Water and Infrastructure, Muthgasse 18, 1190 Vienna, Austria
Christine Stumpp
BOKU University, Institute of Soil Physics and Rural Water Management, Department of Landscape, Water and Infrastructure, Muthgasse 18, 1190 Vienna, Austria
Department of Water Management, Faculty of Civil Engineering and Geosciences, Delft University of Technology, Stevinweg 1, 2628CN Delft, the Netherlands
BOKU University, Institute of Hydrology and Water Management (HyWa), Department of Landscape, Water and Infrastructure, Muthgasse 18, 1190 Vienna, Austria
BOKU University, Institute of Soil Physics and Rural Water Management, Department of Landscape, Water and Infrastructure, Muthgasse 18, 1190 Vienna, Austria
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Total article views: 3,693 (including HTML, PDF, and XML)
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Total article views: 2,721 (including HTML, PDF, and XML)
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Using advances in transit time estimation and tracer data, we tested if fast-flow transit times are controlled solely by soil moisture or if they are also controlled by precipitation intensity. We used soil-moisture-dependent and precipitation-intensity-conditional transfer functions. We showed that a significant portion of event water bypasses the soil matrix through fast flow paths (overland flow, tile drains, preferential-flow paths) in dry soil conditions for both low- and high-intensity precipitation.
Using advances in transit time estimation and tracer data, we tested if fast-flow transit times...