Experimental results for the dynamic surface tension, surface electrization, and for the rate of evaporation (condensation) of water systems are presented.Introduction. "The Niagara has frozen!" This information together with the fascinating pictures of the waterfall in America appeared on the Internet in mid-January, 2014 ( Fig. 1) [1]. The explanation of this phenomenon is that at the place of a sharp change in the liquid fl ow, separate parts of its vertical jets intermix and the elements of its bulk structure appear on the liquid surface. As the experiments carried out by Hiekman [2] showed ( Fig. 2), as the rate of evaporation from a fresh liquid surface increases, the infl uence of the gases near its moving surface is reduced considerably, and the cooling of the liquid increases drastically.The icing of a rapidly fl owing, freshly formed surface of water can be explained by taking into account its peculiar properties under dynamic conditions. The properties of the interface exert a substantial effect on the progress of a large variety of natural processes, including also the evaporation-condensation kinetics that determines the operation of machines and apparatuses, evaporator systems, distillers, and other facilities. In designing industrial apparatuses, the molecular phenomena occurring on the interfaces are to be taken into account in heat and mass transfer calculations.Dynamic Surface Tension. The dynamic surface tension is the tension of a freshly formed nonequilibrium surface of a liquid jet, bubbles, and droplets. An experimental investigation of the dynamic surface tension was carried out by the methods of an oscillating jet and of a maximum pressure in a gaseous bubble with some improvements made in the technique of measurements with account for the liquid fl ow velocity profi le and for the recovery of the forming surface [3]. Water, a number of solutions of inorganic salts, surfactant solutions, dimethylformamide, and other substances were investigated.The most interesting, stably recurring feature of the dynamic surface tension is the temperature inversion: at a very early age of the surface (t = 1-3 ms) and a low concentration of a solution in the temperature range 10-25 o C, the surface tension increases with temperature T. The data for water are presented in Fig. 3 [3].The temperature inversion was observed at a young age of the surface for water and water solution of NaCl in the early works of Schmidt and Steyer [4], as well as Kleinman [5], who used the method of a falling meniscus to measure the dynamic surface tension. The measurements made by Owens [6] for a NaCl solution by the method of an oscillating jet also show that at short times the temperature inversion is possible. On increase in the temperature up to 10 o C and above, the surface tension increases and then decreases.Special experiments with a water jet showed that heating of the jet up to 40-50 o C leads to an equilibrium value of surface tension. For water, the temperature in the region of 30-40 o C is known as the Mendeleev ...