Electrochemical systems provide a fascinating insight into the dynamic interplay of charged species within various phases. One notable example is the interaction between a membrane permeable to K⁺ ions but not to Cl⁻ ions, separating an aqueous KCl solution from pure water. As K⁺ ions diffuse through the membrane, they generate net charges on each phase, leading to a potential difference between them.
Similarly, when a piece of Zn is immersed in an aqueous ZnSO₄ solution, the Zn metal, composed of Zn²⁺ ions and mobile valence electrons, undergoes a dynamic equilibrium where the rates of Zn²⁺ leaving and entering the metal become equal. This results in a net negative charge on the Zn, creating a potential difference (ΔΦ) between the metal and the solution.
The charge associated with Zn²⁺ ions crossing 1 cm² of the metal–solution interface in 1 s, known as the exchange current, is 2 × 10−⁵ C. Utilizing the charge on one proton (e = 1.60218 x 10−19 C) and the Avogadro constant (NA = 6.02214 x 1023 mol−1), the Faraday constant (F) is determined; F = NAe = 96485 C/mol.
The charge on a particle of species i is zie, where zi is the charge number. Therefore, the charge per mole of species i is ziF, and the charge on ni moles of i is Qi = ziFni.
The magnitude and sign of ΔΦ depend on several factors, including temperature, pressure, the nature of the metal, the solvent, and the concentrations of metal ions in the solution.
An example involving Cu and Zn demonstrates that even though solid ions don't diffuse significantly, electrons can move freely between metals, leading to a net charge on each metal at equilibrium. This phenomenon, discovered by Galvani and Volta in the 1790s, has practical applications, such as in thermocouples that utilize the temperature-dependent interphase potential difference to measure temperature.
Electrochemical systems involve a difference in electric potential between two or more phases at equilibrium, where no net chemical transfer occurs, and the potential difference reflects only the electric potential; otherwise, both electric and chemical potentials influence the system. Besides charge transfer, factors like water molecule orientation, electron distribution, and ion distribution contribute to ΔΦ. The potential difference can even arise without charge transfer, as seen in a two-phase system of immiscible liquids. While measuring ΔΦ directly between phases in contact is challenging due to the creation of new interfaces, statistical-mechanical models offer a means to calculate ΔΦ if the distribution of charges and dipoles in the interphase region is known.
Electrochemical systems involve an electric potential difference, ΔΦ, between two or more phases.
For instance, when zinc metal is immersed in a dilute zinc sulfate solution, the low concentration of Zn²⁺ ions drives zinc atoms to dissolve into the solution, leaving electrons behind in the metal, resulting in a net negative charge on the zinc.
This dynamic process at equilibrium establishes a potential difference between the zinc and the solution, and these moving ions carrying charge form an exchange current.
The number of moles of ions carrying this charge can be determined using the Faraday constant, which is the charge per mole of electrons.
So, the charge on ni moles of species i is the product of the charge number, the Faraday constant, and ni.
The magnitude and sign of ΔΦ depend on factors like temperature, pressure, the nature of the metal, the solvent, and ion concentrations.
Similarly, electron movement between metals like copper and zinc can create a net charge at equilibrium, a phenomenon used in thermocouples, which measure temperature through interphase potential differences.
Measurement of ΔΦ is viable only between phases that are in equilibrium.