ABSTRACT
This work is the result of a collaboration between Spanish and Portuguese laboratories. The specific objective was to quantify the time evolution during 1994, 1995 and 1996 of the radioecological impact of the liquid releases of 3H from the Almaraz Nuclear Power Plant (ANPP) in the section of the Tagus River corresponding to Cáceres province in Spain and the Alentejo region in Portugal. We found that the temporal evolution of the levels of tritium depends on the management of the water held in the cooling reservoir of the ANPP and the presence of the dams that exist along the river. This management regime has a 12-month period. Also the movement of the mass of tritiated water (HTO) downriver was much faster during 1996 than 1995 or 1994 due to the hydrological differences between those years and consequently to the different amounts of water transferred between the reservoirs of the dams. From the hypothesis that hydrodynamically it is impossible to differentiate tritiated water from non-tritiated water, a model was constructed that satisfactorily reproduces the temporal evolution of the 3H in the zone of the Tagus River in which the exchange of water takes place, with the cooling reservoir of the Almaraz Nuclear Power Plant.
