SUMMARY
The pH of water in a limestone quarry, specifically involving calcium carbonate (CaCO3), can be calculated using the dissociation constants of carbonic acid (H2CO3) with pKa1=6.37 and pKa2=10.32. The relevant equation is pH = pKa + log [conjugate base]/[acid]. The calculation involves determining hydroxide ion concentration ([OH-]) from the equilibrium expression for bicarbonate (HCO3-) and carbonate (CO3 2-), leading to a pH value of approximately 12.02. The initial concentration of carbonates significantly influences the pH, complicating the determination due to the solubility product of calcium carbonate.
PREREQUISITES
- Understanding of acid-base chemistry and pH calculations
- Familiarity with the dissociation constants (pKa) of weak acids
- Knowledge of carbonate chemistry, including bicarbonate and carbonate ions
- Basic grasp of equilibrium expressions in chemical reactions
NEXT STEPS
- Study the solubility product constant (Ksp) of calcium carbonate (CaCO3)
- Learn about the hydrolysis of carbonates and its effect on pH
- Explore the concept of amphiprotic salts and their pH calculations
- Review the application of the Henderson-Hasselbalch equation in buffer solutions
USEFUL FOR
Chemistry students, environmental scientists, and professionals involved in water quality assessment in limestone quarry operations.