Grundwassererneuerung durch Interflow in Abhängigkeit von Bodenfeuchte und Niederschlag. in Wasserhaushalt und Gewässer. Festschrift zum 60. Geburtstag von Professor Dr. Reiner Keller.. (Groundwater recharge from interflow in dependence on soil
Untersuchungen zum Problem des Interflow. Messungen der Bodenfeuchte, der Hangwasserbewegung, der Grundwassererneuerung und des Abflussverhaltens im Versuchsgebiet Hollmuth/Kleiner Odenwald. (Investigations to the problem of interflow. Measurement
of the soil-moisture, of the interflow in the slope, of the renewal of groundwater and of the run-off regime on the test field of Hollmuth, Kleiner Odenwald)
Après avoir exposé ce qu'on entend par interflow (écoulement hypodermique: écoulement subsuperficiel de l'eau de versant, facteur de renouvellement de l'eau souterraine), par écoulement et par bilan hydrologique, l'A. décrit les méthodes et les
This paper examines the relationship between interflow, groundwater recharge and stream discharge, based on empirical investigations at the Hollmuth test field.
by a complex of geomorphic processes involving frost weathering, episodic or periodic aquatic transport and deposition in connection with surface runoff, slopewash and active layer interflow. (l'A.).
conception d'ensemble des études conduites depuis 1975 est fondée sur un établissement du bilan de gestion de la nature centré autour des eaux courantes. Rapports sur l'interflow/écoulement moyen, la gestion de l'eau du sol, l'écoulement superficiel et le
Within the hydrological cycle the unsaturated part of the soil matrix represents the most important transformation link of precipitation into overland flow, interflow and groundwater flow. Therefore, the simulation of flow processes in the system
of overland- and interflow and increased risk of overtopping of dams during extreme rainfall events. The lessons learned are being used to improve blocking strategies and dam design. The changes in peatland topography caused by drainage, however, need