The starting points for the definition of an EF in both methods are the basic hydrological and hydraulic parameters, such as the mean annual flow, the mean minimum flow, the minimum flow, etc. Where there is very limited, or no hydrological data, it has been suggested that hydrological observations should be carried out for two years for new water abstractions, especially in the minimal flow periods.
The Ministry of the Environment and Spatial Planning required that EFAs be undertaken on all running waters, where an EF had not yet been specified. As a result, from 1992 the EF was assessed for more than 180 sections of running waters in Slovenia according to the methods described above. Most of EFs were assessed for the existing water users (123 study sites).
The independent researches involved in developing the criteria for EF played a major role in the programme of studies to determined most values of EF in Slovenia. The time needed to complete a particular study varied from a few months for small streams to two years for larger rivers. The EFA sought to increase water flow in the riverbed in a manner improved conditions for organisms in the water and in the riparian zone. This typically meant that especially in the low-flow periods, smaller quantities of water could be abstracted from the running waters.
For most small streams, the EF was determined according to the hydrological method. For the rivers with large water abstractions, the value of EF was mostly determined according to the ecological method. If it was possible, experiments were made with trial increases of the flows downstream of dams and the evaluation of habitats at different flows.