Phase equilibria

Why does ice melt under a skater's blade but not under a resting shoe? Why does water boil at a lower temperature on a mountain top than at the seaside? Both questions have the same answer: the boundary between two phases of a pure substance on a pressure-temperature map is not drawn by guesswork, it is fixed by a single equality condition — the chemical potential of each phase must match wherever the phases coexist. This article makes that condition quantitative for one-component systems: the Gibbs phase rule counts how much freedom is left once you specify how many phases coexist, and the Clausius–Clapeyron equation derives the exact slope of every coexistence curve on the phase diagram. Together they explain the shape of the everyday water phase diagram — including why its melting curve tilts the "wrong" way — from chemical-potential equality alone, with no new postulate needed.

The core insight

Equality of chemical potential between two coexisting phases of a pure substance, μ(α)=μ(β)\mu^{(\alpha)}=\mu^{(\beta)}, fixes both how many degrees of freedom remain (Gibbs phase rule F=C−P+2F=C-P+2) and the exact slope dP/dT=ΔHtrs/(TΔVtrs)dP/dT=\Delta H_{trs}/(T\Delta V_{trs}) of every phase boundary (Clausius–Clapeyron equation).

The core idea

Counting freedom with the Gibbs phase rule. For a system with CC independent components and PP phases coexisting in equilibrium, the number of intensive variables (like TT and PP) that can still be varied independently without disturbing which phases are present is

F=C−P+2F = C - P + 2

where: CC is the number of independent components, PP is the number of coexisting phases, and 22 counts temperature and pressure as the two intensive variables available in a pure PVTPVT system. For a one-component system (C=1C=1), a single phase gives F=2F=2 — a full 2-D region of the phase diagram where both TT and PP roam freely. Two phases in equilibrium give F=1F=1 — a 1-D curve, where choosing TT fixes PP. Three phases together give F=0F=0 — a single unmovable point.

Deriving the boundary slope. Along any two-phase coexistence curve, μ(α)(T,P)=μ(β)(T,P)\mu^{(\alpha)}(T,P)=\mu^{(\beta)}(T,P) holds at every point on the curve, not just one. Differentiating this equality using dμ=−Sm dT+Vm dPd\mu=-S_m\,dT+V_m\,dP per mole (from dG=−S dT+V dPdG=-S\,dT+V\,dP) for each phase, and using ΔStrs=ΔHtrs/Ttrs\Delta S_{trs}=\Delta H_{trs}/T_{trs} for a reversible transition, gives the Clausius–Clapeyron equation:

dPdT=ΔStrsΔVtrs=ΔHtrsT ΔVtrs\frac{dP}{dT} = \frac{\Delta S_{trs}}{\Delta V_{trs}} = \frac{\Delta H_{trs}}{T\,\Delta V_{trs}}

where: ΔHtrs\Delta H_{trs} and ΔVtrs\Delta V_{trs} are the molar enthalpy and volume change on crossing the boundary (fusion, vaporisation, or sublimation), and TT is the coexistence temperature. This single formula is valid for any of the three boundaries on a one-component phase diagram — only the transition being described changes.

Integrating for the vapour branches. When a gas phase is involved, ΔVtrs≈Vm(gas)=RT/P\Delta V_{trs}\approx V_m^{(gas)}=RT/P (the condensed-phase volume is negligible by comparison), so the Clausius–Clapeyron equation becomes a separable differential equation in PP and TT that integrates, for roughly constant ΔHvap\Delta H_{vap}, to

ln⁡P2P1=−ΔHvapR(1T2−1T1)\ln\frac{P_2}{P_1} = -\frac{\Delta H_{vap}}{R}\left(\frac{1}{T_2}-\frac{1}{T_1}\right)

where: P1,T1P_1,T_1 is one known vapour-pressure/temperature point, P2,T2P_2,T_2 is the point you want, and R=8.314 J mol−1K−1R=8.314\ \text{J mol}^{-1}\text{K}^{-1}. This lets you predict vapour pressure at a new temperature from one reference point, or extract ΔHvap\Delta H_{vap} from two measured points.

Figure
A pressure temperature phase diagram for a pure substance with three regions solid liquid and vapour meeting at a triple point and the liquid vapour curve ending at a critical point
One-component P-T phase diagram temperature T pressure P sublimation fusion curve vaporisation triple point F=0 critical point solid F=2 liquid F=2 vapour F=2
Derivation AVapour pressure of water at a lower temperature from the Clausius-Clapeyron equation

The goal is to show, using only integration of a separable differential equation and one exponentiation, how a single known boiling point converts into the full vapour-pressure-versus-temperature curve, so that any other point on that curve — such as water's vapour pressure below its normal boiling point — follows from arithmetic alone.

Step 1. Start from the integrated Clausius–Clapeyron equation with the gas-dominant approximation ΔVtrs≈Vm(gas)=RT/P\Delta V_{trs}\approx V_m^{(gas)}=RT/P already substituted: ln⁡P2P1=−ΔHvapR(1T2−1T1)\ln\dfrac{P_2}{P_1} = -\dfrac{\Delta H_{vap}}{R}\left(\dfrac{1}{T_2}-\dfrac{1}{T_1}\right). Treat T1,P1T_1,P_1 as the known reference (water's normal boiling point) and T2T_2 as the temperature of interest.

Step 2. Compute the temperature term. With T1=373.15 KT_1=373.15\ \text{K} and T2=363.15 KT_2=363.15\ \text{K}: 1363.15=2.7538×10−3 K−1\dfrac{1}{363.15}=2.7538\times10^{-3}\ \text{K}^{-1} and 1373.15=2.6799×10−3 K−1\dfrac{1}{373.15}=2.6799\times10^{-3}\ \text{K}^{-1}, so the bracket (1T2−1T1)=7.39×10−5 K−1\left(\dfrac{1}{T_2}-\dfrac{1}{T_1}\right)=7.39\times10^{-5}\ \text{K}^{-1}.

Step 3. Multiply by −ΔHvap/R-\Delta H_{vap}/R with ΔHvap=40,700 J mol−1\Delta H_{vap}=40{,}700\ \text{J mol}^{-1}: ln⁡P2P1=−407008.314×7.39×10−5=−4895.6×7.39×10−5=−0.3618\ln\dfrac{P_2}{P_1} = -\dfrac{40700}{8.314}\times7.39\times10^{-5} = -4895.6\times7.39\times10^{-5} = -0.3618.

Step 4. Exponentiate to undo the logarithm and solve for P2P_2: P2P1=e−0.3618=0.6965\dfrac{P_2}{P_1}=e^{-0.3618}=0.6965, so with P1=101,325 PaP_1=101{,}325\ \text{Pa} (1 atm), P2=0.6965×101,325=70,590 Pa≈0.697 atmP_2 = 0.6965\times101{,}325 = 70{,}590\ \text{Pa}\approx0.697\ \text{atm}. This matches the direct calculation in the worked example, confirming the integrated formula reproduces the reference point-to-point result.

Worked example

Water's normal boiling point is 373.15 K373.15\ \text{K} at 1 atm1\ \text{atm}, and its molar enthalpy of vaporisation is ΔHvap=40.7 kJ mol−1\Delta H_{vap}=40.7\ \text{kJ mol}^{-1}. Estimate the vapour pressure of water at 363.15 K363.15\ \text{K} (90∘C90^\circ\text{C}), then use the Gibbs phase rule to explain why this vapour-pressure curve is a line, not a region, on the phase diagram.

Step 1. Apply the integrated Clausius–Clapeyron equation: ln⁡P2P1=−407008.314(1363.15−1373.15)=−4895.6×7.39×10−5=−0.3618\ln\dfrac{P_2}{P_1} = -\dfrac{40700}{8.314}\left(\dfrac{1}{363.15}-\dfrac{1}{373.15}\right) = -4895.6\times7.39\times10^{-5} = -0.3618.

Step 2. Exponentiate: P2P1=e−0.3618=0.6965\dfrac{P_2}{P_1}=e^{-0.3618}=0.6965, so P2=0.6965×101,325 Pa=70,590 Pa≈0.697 atmP_2 = 0.6965\times101{,}325\ \text{Pa} = 70{,}590\ \text{Pa}\approx\mathbf{0.697\ atm}. This is close to the experimental ≈0.692 atm\approx0.692\ \text{atm} at 90∘C90^\circ\text{C}; the small gap comes from treating ΔHvap\Delta H_{vap} as constant and the vapour as ideal.

Step 3. Apply the Gibbs phase rule to the liquid-vapour boundary: two phases coexist (Pphases=2P_{phases}=2) for a one-component system (C=1C=1), so F=1−2+2=1F=1-2+2=1. One degree of freedom means choosing TT fixes PP — you cannot pick both independently and stay on the boundary — which is exactly why the vaporisation curve traced by the equation above is a 1-D curve, not a 2-D region. The vapour pressure at 90∘C90^\circ\text{C} is about 0.697 atm0.697\ \text{atm}, and F=1F=1 on that curve confirms TT alone determines it.

Competitive stretch

At the triple point of water, three phases coexist simultaneously (Pphases=3P_{phases}=3), so F=1−3+2=0F=1-3+2=0: neither TT nor PP can be varied at all without losing a phase, pinning the triple point to a unique (273.16 K, 611.657 Pa)(273.16\ \text{K},\ 611.657\ \text{Pa}) — the reason it is used as a fixed calibration reference for temperature scales.

Common traps

  • Applying ΔVtrs≈Vm(gas)\Delta V_{trs}\approx V_m^{(gas)} (valid for vaporisation/sublimation) to the fusion curve — both phases there are condensed, so ΔVfus\Delta V_{fus} is small and can even be negative, which is why ice's melting curve has a negative slope via dP/dT=ΔHfus/(TΔVfus)dP/dT=\Delta H_{fus}/(T\Delta V_{fus}).
  • Confusing "FF degrees of freedom" with a count of phases or components — FF counts independently variable intensive variables like TT and PP, not how many substances or phases are present.
  • Treating ΔHvap\Delta H_{vap} as truly constant over a wide temperature range in the integrated equation — it shrinks toward zero as TT approaches the critical point, where the phase distinction itself disappears.
  • Trying to extend this one-component treatment to binary or ternary alloy phase diagrams — CY11001 scopes this topic to pure substances; multi-component phase diagrams need a different framework.

Ask the tutor: if the step from μ(α)=μ(β)\mu^{(\alpha)}=\mu^{(\beta)} along a curve to the Clausius–Clapeyron slope formula felt rushed, ask the AI tutor to expand dμ(α)=dμ(β)d\mu^{(\alpha)}=d\mu^{(\beta)} term by term.

Why does water boil at a lower temperature on a mountain top?

Atmospheric pressure is lower at altitude, and boiling happens exactly when the liquid's vapour pressure equals the surrounding pressure. Reading the vaporisation curve backwards from the Clausius–Clapeyron equation, a lower target pressure P2P_2 corresponds to a lower temperature T2T_2 — so the same water boils at, say, 90∘C90^\circ\text{C} instead of 100∘C100^\circ\text{C} where the local atmospheric pressure matches roughly 0.697 atm0.697\ \text{atm}, exactly the value computed in the worked example above.

Why is the Gibbs phase rule written with a plus 2 rather than just C minus P?

The +2+2 accounts for the two intensive variables, temperature and pressure, that describe a pure PVTPVT system before any phase-coexistence constraints are applied. Each additional phase in equilibrium imposes one more chemical-potential-equality constraint (μ(α)=μ(β)\mu^{(\alpha)}=\mu^{(\beta)}), which removes one degree of freedom — hence subtracting PP. Composition variables would add further terms in a multi-component system, but for C=1C=1 the +2+2 alone captures the full starting freedom.

Can I use the integrated Clausius-Clapeyron equation for melting instead of boiling?

Not with the simplification used here. That integrated form relies on ΔVtrs≈Vm(gas)=RT/P\Delta V_{trs}\approx V_m^{(gas)}=RT/P, which is only valid when one phase is a gas whose volume dwarfs the condensed phase's volume — true for vaporisation and sublimation, but not for fusion, where both phases are condensed and comparable in volume. For the fusion curve you must keep the original differential form dP/dT=ΔHfus/(TΔVfus)dP/dT=\Delta H_{fus}/(T\Delta V_{fus}) with the actual (small, sometimes negative) ΔVfus\Delta V_{fus}.

Before this

Where this leads