SUMMARY
The discussion focuses on calculating the standard Gibbs free energy change (ΔG°) for the ionization of water at 50°C, where the pH of pure water is 6.55. The equilibrium constant (Keq) is derived from the hydronium ion concentration, calculated as [H+] = 10^[-6.55] = 2.8*10^-7. Using the equation ΔG° = -RTln(Keq), the calculated ΔG° is 81.00 kJ/mol. The participants confirm the assumption of equilibrium at this temperature.
PREREQUISITES
- Understanding of Gibbs free energy and its equations
- Knowledge of pH and hydronium ion concentration calculations
- Familiarity with equilibrium constants (Keq) in chemical reactions
- Basic thermodynamics, specifically the relationship between temperature and Gibbs free energy
NEXT STEPS
- Research the impact of temperature on the ionization of water
- Learn about the relationship between pH and pKa values in aqueous solutions
- Explore the concept of chemical equilibrium and its applications in thermodynamics
- Study the derivation and implications of the Gibbs free energy equation in various chemical contexts
USEFUL FOR
Chemistry students, educators, and researchers interested in thermodynamics and the properties of water at varying temperatures.