SUMMARY
The discussion focuses on calculating the melting point of ice under a pressure of 6000 kPa using the Clausius–Clapeyron relation. Participants emphasize the importance of using the densities of solid and liquid water, approximately 920 kg/m3 and 1000 kg/m3, respectively, to determine the volume change during melting. The correct approach involves applying the melting version of the Clausius–Clapeyron equation, not the evaporation version, to find the change in temperature (delta T). The final melting point can be calculated by adjusting the standard melting point of water with the derived delta T.
PREREQUISITES
- Understanding of the Clausius–Clapeyron relation
- Knowledge of density calculations for solids and liquids
- Familiarity with thermodynamic concepts such as heat of fusion
- Basic algebra for rearranging equations
NEXT STEPS
- Study the Clausius–Clapeyron relation specifically for phase changes
- Learn how to calculate volume changes using density values
- Research the heat of fusion for various substances
- Practice solving problems involving pressure and phase transitions
USEFUL FOR
Students in chemistry or physics, educators teaching thermodynamics, and anyone interested in the effects of pressure on phase changes of water.