General Chemistry II · Intermolecular Forces Liquids Solids

The Clausius–Clapeyron Equation

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On this page 8 sections
  1. In 30 seconds
  2. Why this matters
  3. The college version
  4. Eli explains
  5. Worked example
  6. Key takeaway
  7. Study tools
  8. Sources & references

In 30 seconds

The Clausius–Clapeyron equation quantifies how a liquid's vapor pressure rises with temperature. Because vaporization is endothermic, more molecules can escape at higher temperature, and the relationship is exponential. In its two-point form, ln(P₂/P₁) = −(ΔHᵥₐₚ/R)(1/T₂ − 1/T₁), the equation lets you calculate the vapor pressure at one temperature if you know it at another, given the enthalpy of vaporization ΔHᵥₐₚ.

Why this matters

  • Meteorology: relates humidity, dew point, and saturation vapor pressure to temperature.
  • Boiling at altitude / pressure cooking: predicts boiling points at non-standard pressures.
  • Engineering: design of distillation columns, evaporators, and steam systems.
  • Safety: estimates how much flammable vapor a solvent generates at a given temperature.

The college version

Core Concept

The Clausius–Clapeyron equation quantifies how a liquid's vapor pressure rises with temperature. Because vaporization is endothermic, more molecules can escape at higher temperature, and the relationship is exponential. In its two-point form, ln(P₂/P₁) = −(ΔHᵥₐₚ/R)(1/T₂ − 1/T₁), the equation lets you calculate the vapor pressure at one temperature if you know it at another, given the enthalpy of vaporization ΔHᵥₐₚ.

Key Ideas

The underlying physics

  • Vaporization is endothermic (ΔHᵥₐₚ > 0). Raising temperature shifts the kinetic-energy distribution so more molecules exceed the escape threshold.
  • Vapor pressure therefore increases exponentially, not linearly, with temperature.

The two forms

  • Linear/graphical form: ln P = −(ΔHᵥₐₚ/R)(1/T) + C. A plot of ln P vs. 1/T is a straight line with slope −ΔHᵥₐₚ/R.
  • Two-point form (most used in exams): ln(P₂/P₁) = −(ΔHᵥₐₚ/R)(1/T₂ − 1/T₁).

Assumptions

  • ΔHᵥₐₚ is treated as constant over the temperature range (it actually varies slightly with T).
  • Temperatures must be in kelvin; pressures may be in any consistent units.
  • Valid below the critical point, away from extreme conditions.

Equations and Variables

  • Clausius–Clapeyron (two-point): ln(P₂/P₁) = −(ΔHᵥₐₚ/R)(1/T₂ − 1/T₁)
    • P₁, P₂ = vapor pressures at temperatures T₁, T₂ (same units for P)
    • T₁, T₂ = absolute temperatures in kelvin
    • ΔHᵥₐₚ = molar enthalpy of vaporization (J/mol, to match R)
    • R = 8.314 J/(mol·K)
  • Graphical form: ln P = −(ΔHᵥₐₚ/R)(1/T) + C; slope = −ΔHᵥₐₚ/R.

How It Works

  1. Start with known (P₁, T₁). You typically know the normal boiling point (T where P = 1 atm) or a tabulated vapor pressure.
  2. Convert temperatures to kelvin. T(K) = T(°C) + 273.15. Using °C gives nonsense results.
  3. Make units consistent. Put ΔHᵥₐₚ in J/mol so it cancels with R = 8.314 J/mol·K.
  4. Compute the exponent. Evaluate (1/T₂ − 1/T₁), multiply by −ΔHᵥₐₚ/R.
  5. Solve. Exponentiate to find P₂/P₁, then P₂. To find a boiling point at a given pressure, solve for T₂ instead.

Worked Example

The normal boiling point of water is 100 °C (P₁ = 760 torr at T₁ = 373.15 K), and ΔHᵥₐₚ = 40.7 kJ/mol. Estimate the vapor pressure of water at 25 °C.

  1. Convert. T₁ = 373.15 K, T₂ = 25 + 273.15 = 298.15 K, ΔHᵥₐₚ = 40,700 J/mol.
  2. Compute 1/T₂ − 1/T₁. 1/298.15 − 1/373.15 = 0.003354 − 0.002680 = 0.000674 K⁻¹.
  3. Compute the exponent. −(ΔHᵥₐₚ/R)(1/T₂ − 1/T₁) = −(40,700 / 8.314)(0.000674) = −(4895)(0.000674) = −3.30.
  4. Exponentiate. ln(P₂/760) = −3.30 → P₂/760 = e⁻³·³⁰ = 0.0369.
  5. Solve. P₂ = 760 × 0.0369 = 28 torr (measured value ≈ 23.8 torr; the small difference reflects ΔHᵥₐₚ varying with temperature).

How it works

  1. Start with known (P₁, T₁). You typically know the normal boiling point (T where P = 1 atm) or a tabulated vapor pressure.
  2. Convert temperatures to kelvin. T(K) = T(°C) + 273.15. Using °C gives nonsense results.
  3. Make units consistent. Put ΔHᵥₐₚ in J/mol so it cancels with R = 8.314 J/mol·K.
  4. Compute the exponent. Evaluate (1/T₂ − 1/T₁), multiply by −ΔHᵥₐₚ/R.
  5. Solve. Exponentiate to find P₂/P₁, then P₂. To find a boiling point at a given pressure, solve for T₂ instead.

Common confusions

  • "I can use Celsius in the equation." — Wrong. The 1/T terms must use absolute temperature (kelvin); Celsius gives incorrect ratios.
  • "Any unit for ΔHᵥₐₚ works." — Wrong. Use J/mol to match R = 8.314 J/mol·K (or kJ/mol with R = 0.008314 kJ/mol·K).
  • "The two pressures can be in different units." — Wrong. P₁ and P₂ must share the same units (they cancel in the ratio).
  • "Vapor pressure rises linearly with temperature." — Wrong. It rises exponentially (hence the ln form).
  • "The slope is +ΔHᵥₐₚ/R." — Wrong. The slope of ln P vs. 1/T is negative, −ΔHᵥₐₚ/R.

Quick review

  • Two-point form: ln(P₂/P₁) = −(ΔHᵥₐₚ/R)(1/T₂ − 1/T₁).
  • Use kelvin; use consistent pressure units; ΔHᵥₐₚ in J/mol.
  • ln P vs. 1/T is linear with slope −ΔHᵥₐₚ/R.
  • Worked: water, 760 torr at 373 K → ≈28 torr at 298 K.
Eli, the EliExplains learning guide

Eli explains

The same idea, in plain words

Explain it like I’m 10

Vapor pressure is like how many kids are jumping out of a bouncy castle. When it's warm, everyone is bouncing higher, so way more kids fly out over the walls. The rule that tells you exactly how many more kids fly out when you turn the heat up a little is the Clausius–Clapeyron equation. The "hill" the kids have to climb to escape is ΔHᵥₐₚ (the energy to vaporize) — the taller the hill, the more dramatically the number of escapees changes with temperature. (The analogy's limit: the equation doesn't count individual kids; it predicts the ratio of pressures at two temperatures, and it assumes the "hill height" doesn't change, which is only approximately true.)

Worked example

Worked Example

The normal boiling point of water is 100 °C (P₁ = 760 torr at T₁ = 373.15 K), and ΔHᵥₐₚ = 40.7 kJ/mol. Estimate the vapor pressure of water at 25 °C.

  1. Convert. T₁ = 373.15 K, T₂ = 25 + 273.15 = 298.15 K, ΔHᵥₐₚ = 40,700 J/mol.
  2. Compute 1/T₂ − 1/T₁. 1/298.15 − 1/373.15 = 0.003354 − 0.002680 = 0.000674 K⁻¹.
  3. Compute the exponent. −(ΔHᵥₐₚ/R)(1/T₂ − 1/T₁) = −(40,700 / 8.314)(0.000674) = −(4895)(0.000674) = −3.30.
  4. Exponentiate. ln(P₂/760) = −3.30 → P₂/760 = e⁻³·³⁰ = 0.0369.
  5. Solve. P₂ = 760 × 0.0369 = 28 torr (measured value ≈ 23.8 torr; the small difference reflects ΔHᵥₐₚ varying with temperature).

Key takeaways

  • ### High-Yield Facts
  • ln(P₂/P₁) = −(ΔHᵥₐₚ/R)(1/T₂ − 1/T₁).
  • Temperatures MUST be in kelvin.
  • ΔHᵥₐₚ in J/mol matches R = 8.314 J/mol·K.
  • Slope of ln P vs. 1/T is −ΔHᵥₐₚ/R.
  • Larger ΔHᵥₐₚ → steeper slope → vapor pressure changes more with temperature.
  • The equation assumes constant ΔHᵥₐₚ (an approximation).

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Practice General Chemistry II

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Study tools & related lessonsYou’ll learn to · Related

You’ll learn to

  • State the two-point (integrated) form of the Clausius–Clapeyron equation.
  • Use it to find a vapor pressure at a new temperature (or a temperature at a new pressure).
  • Explain why the equation requires absolute (Kelvin) temperatures and constant ΔHᵥₐₚ.
  • Interpret the slope of a plot of ln P versus 1/T.

Sources & references

  1. OpenStax, *Chemistry 2e*, "10.3 Phase Transitions." https://openstax.org/books/chemistry-2e/pages/10-3-phase-transitions
  2. NIST Chemistry WebBook, "Water." https://webbook.nist.gov/cgi/cbook.cgi?ID=C7732185
  3. NIST Chemistry WebBook. https://webbook.nist.gov/chemistry/
  4. OpenStax, *Chemistry 2e* (book home). https://openstax.org/details/books/chemistry-2e
  5. PubChem, "Water" (compound 962). https://pubchem.ncbi.nlm.nih.gov/compound/962

This lesson was adapted from the open educational references above; their licenses and attributions are preserved. See Copyright & Licensing.

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