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Yakov I. Korepanov

Publications and source records attributed to Yakov I. Korepanov.

2 recordsLinked to original sources

Equilibrium in solid-state electrochemical cells at sample-electrolyte boundary

In solid-state electrochemical experiments, the boundary between the sample and the electrolyte plays a crucial role, and the rest of the sample acting as a buffer that maintains a fixed composition. Due to the presence of an electrochemical circuit in the cell (ionic conductivity in the electrolyte and electronic conductivity in the sample system), the chemical potential is equalized at the electrolyte-sample boundary. This leads to an equilibrium state and allows for the measurement of equilibrium values, regardless of the assumptions made by the experimenters. This article demonstrates the principle of equalizing the electrochemical potential at the electrolyte-sample interface, which explains why achieving equilibrium in the presence of an electrolyte can occur much faster compared to sample synthesis, which often occurs at higher temperatures. This fact can be used to synthesize sample systems or other substances at the required temperatures with a significant reduction in synthesis time.

cond-mat.mtrl-sci↗

Theoretical demonstration of the possibility of using binary alloys or solid solutions in ternary systems as geothermometers

The investigation of the processes of mineral deposit formation and their history is a fundamental task. Solving this task can increase mining efficiency and make a significant contribution to understanding the formation of the Earth's crust. The main approach to solving this task is determining the values of thermodynamic functions for phases present in deposits. One of the most promising and flexible methods for studying thermodynamic properties is the EMF method. This article describes the basic principles of the EMF method and provides all possible interpretations of the obtained results. It has also been demonstrated that direct EMF measurements can determine the composition of a solid solution or alloy in a multicomponent system if its EMF dependencies are known. Based on this fact, it can be concluded that any alloy or solid solution in a multi-phase association, which undergoes composition changes with temperature and can be quenched, can be used as a geothermometer or geobarometer.

cond-mat.mtrl-sci↗