In the partial catchment basins and on the experimental slope within the Homerka drainage basin there was carried out a series of measurements of the quantity and quality of water during a summer drought. Close relationships were found to exist
rate of streamflow and rate of denudation are expressed by a hyperbola equation which can be written: y = ax + b/x. It may be accepted as a mathematical model of the areal hydrologic variability in the drainage basins of the flysch Carpathians. (D'après