SUMMARY
The pH of pure water at 10°C, where the pKw is 14.54, is calculated to be 7.27. This is derived from the equation [H+]^2 = 10^-14.54, which represents the relationship between hydrogen ion concentration and hydroxide ion concentration in water. The pH scale is logarithmic, indicating that each unit change represents a tenfold change in hydrogen ion concentration. It is crucial to understand that the pH scale can extend beyond the conventional range of 0 to 14, allowing for negative values.
PREREQUISITES
- Understanding of pKw and its significance in acid-base chemistry
- Familiarity with the dissociation of water and the relationship between [H+] and [OH-]
- Knowledge of logarithmic functions and their application in pH calculations
- Basic concepts of acid-base equilibrium and electroneutrality
NEXT STEPS
- Study the derivation and implications of pKw in different temperatures
- Learn about the calculation of pH in solutions with varying concentrations of acids and bases
- Explore the concept of electroneutrality in aqueous solutions
- Investigate the behavior of pH in non-standard conditions, including extreme pH values
USEFUL FOR
Chemistry students, educators, and professionals in fields related to environmental science, water quality analysis, and chemical engineering will benefit from this discussion.