Frédéric Perrier, Thierry Héritier and Jean Aupiais
Département Analyse, Surveillance, Environnement, Commissariat à l’Energie Atomique
BP12, F-91680 Bruyères-Le-Châtel, France
Umesh Gautam, Gyani Raja Chitrakar, Prithvi Shrestha and Basanta Kafle
National Seismological Centre, Department of Mines and Geology
Lainchaur, Kathmandu, Nepal
The Dhor Barahi spring in Tanahun district, Western Nepal, is characterised by intermittent periodic flow or unsteady continuous flow, depending on the time of the year. This behaviour can be attributed to a siphon that can be constrained by the local geology and water chemistry data. During periodic discharges, electrical signals are observed with an amplitude proportional to the water flow rate, as predicted by the electrokinetic effect, with a maximum coupling of -1.3±0.3 Vsm-3. The spatial structure of the surface potential leads to a qualitative description of the electrical sources, also compatible with an electrokinetic mechanism, but additional contributions are possible. This study illustrates how combined geochemical and electrical measurements can provide access to the dynamics of groundwater circulation, with possible implications for the monitoring of hydrological, tectonic or volcanic processes.
