Geoelectric Monitoring of a Tracer Experiment at Haslemoen, Norway, during the Winter of 1995

Recent studies have focused on the use of the geoelectrical method to monitor tracer experiments (Bevc and Morrison 1991, Karous 1993, White 1995). Geoelectrical monitoring is suggested as a replacement or as a supplement to traditional tracer experiments, which require taking actual samples of groundwater. The aim of tracer experiments is to determine hydrological parameters such as e.g. groundwater flow direction or velocity of flow.