Clausius-Clapeyron Equation:
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The Clausius-Clapeyron equation describes the relationship between vapor pressure and temperature for a substance. It's particularly useful for determining the enthalpy of vaporization (ΔH) of water or other liquids.
The calculator uses the integrated form of the Clausius-Clapeyron equation:
Where:
Explanation: The equation relates the natural log of the vapor pressure ratio to the inverse temperature difference, scaled by the enthalpy of vaporization.
Details: The enthalpy of vaporization is a crucial thermodynamic property that indicates the energy required to convert a liquid into vapor at constant pressure. It's important for understanding phase transitions, designing distillation systems, and modeling atmospheric processes.
Tips: Enter pressures in Pascals (Pa) and temperatures in Kelvin (K). For water, typical values might be P1=3169 Pa at T1=298K and P2=12280 Pa at T2=323K.
Q1: What are typical ΔH values for water?
A: The enthalpy of vaporization for water is about 40.7 kJ/mol at 100°C, but varies with temperature.
Q2: Why must temperatures be in Kelvin?
A: The equation requires absolute temperature because it involves inverse temperature differences that wouldn't be consistent in Celsius.
Q3: How accurate is this method?
A: It provides reasonable estimates when the temperature range is small and the vapor behaves ideally.
Q4: Can this be used for other liquids?
A: Yes, but the temperature range should be small enough that ΔH remains approximately constant.
Q5: What are limitations of this approach?
A: It assumes ΔH is constant over the temperature range and that the vapor behaves as an ideal gas.