Carbonate melts are successfully applied as supporting electrolytes in the organization of electrolytic separation of heavy metals [1] provided that the melts are minimally involved in the electrode reaction. The carbonate ion at high temperatures is known to dissociate by the reactionThe oxygen ion activity in the melt varies widely as a function of carbon dioxide pressure. The equilibrium acquired on an inert electrode in the anodic potential region [2] is
(B)Under a reducing atmosphere with anodic polarization, hydroxide anions appear in the melt [3]:
(C)All of the specified components of the electrochemical system can participate in adsorption and electrochemical processes, thus determining the energy of the electrode-electrolyte interphase. Here, we elucidate the role of the gas phase over the carbonate electrolyte in the energy state of the interface between a solid electrode and the salt melt.We chose the free energy, which expresses the reversible work of unit surface formation, to characterize the interphase boundary. The free energy was determined by measuring the pulling-in force acting on a solid sample in a wetting liquid [4]. Experiments were carried out on an installation assembled around a Mettler AT-20 electronic balance; the installation is described elsewhere [5]. The installation comprises a weighing device, a precise moving device, an electrochemical cell, and a heating system. The balance is enclosed in a housing that is connected to vacuum and gas systems to create the required atmosphere in the housing and the measurement cell. The cell, whichC O 2 OH -e. + + = comprised a stoppered quartz tube, a gold crucible containing the melt, working and ancillary electrodes, and a reference electrode, was mounted in a temperaturecontrolled heating furnace. The working electrode was suspended on the balance beam. The housing was rigidly mounted to a vertical mover equipped with an indicator (a KM-6 cathetometer), which provided the vertical advance of the working electrode with ∆ h = ± 0.001 mm.The test electrode was weighed first freely hanging ( P 0 ) and then at the moment when it touched the melt ( P ). The weight difference ∆ Pg = W ( g is the gravity acceleration) and the wetting parameter L (a known value) allow us to calculate the increment in the surface formation energy from ∆σ = . The use of a polarizing electrode and a reference electrode in the cell enabled us to study the interphase energy as a function of electric potential. The maximal scatter of data points in one experiment did not exceed 0.5 mJ/m 2 . The precision in a set of experiments was 3%.A high-purity (99.99%) gold cylinder served as a model electrode to record electrocapillarity curves since gold is the most electropositive metal in the test medium and is indifferent to the components of the electrolyte [2]. The electrode potential was set using a potentiostat with reference to an ancillary gold electrode and was measured against an oxygen reference electrode. The latter was a gold wire with a developed surface immersed int...