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.
Equality of chemical potential between two coexisting phases of a pure substance, , fixes both how many degrees of freedom remain (Gibbs phase rule ) and the exact slope of every phase boundary (Clausius–Clapeyron equation).
The core idea
Counting freedom with the Gibbs phase rule. For a system with independent components and phases coexisting in equilibrium, the number of intensive variables (like and ) that can still be varied independently without disturbing which phases are present is
where: is the number of independent components, is the number of coexisting phases, and counts temperature and pressure as the two intensive variables available in a pure system. For a one-component system (), a single phase gives — a full 2-D region of the phase diagram where both and roam freely. Two phases in equilibrium give — a 1-D curve, where choosing fixes . Three phases together give — a single unmovable point.
Deriving the boundary slope. Along any two-phase coexistence curve, holds at every point on the curve, not just one. Differentiating this equality using per mole (from ) for each phase, and using for a reversible transition, gives the Clausius–Clapeyron equation:
where: and are the molar enthalpy and volume change on crossing the boundary (fusion, vaporisation, or sublimation), and 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, (the condensed-phase volume is negligible by comparison), so the Clausius–Clapeyron equation becomes a separable differential equation in and that integrates, for roughly constant , to
where: is one known vapour-pressure/temperature point, is the point you want, and . This lets you predict vapour pressure at a new temperature from one reference point, or extract from two measured points.
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 already substituted: . Treat as the known reference (water's normal boiling point) and as the temperature of interest.
Step 2. Compute the temperature term. With and : and , so the bracket .
Step 3. Multiply by with : .
Step 4. Exponentiate to undo the logarithm and solve for : , so with (1 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 at , and its molar enthalpy of vaporisation is . Estimate the vapour pressure of water at (), 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: .
Step 2. Exponentiate: , so . This is close to the experimental at ; the small gap comes from treating as constant and the vapour as ideal.
Step 3. Apply the Gibbs phase rule to the liquid-vapour boundary: two phases coexist () for a one-component system (), so . One degree of freedom means choosing fixes — 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 is about , and on that curve confirms alone determines it.
Competitive stretch
At the triple point of water, three phases coexist simultaneously (), so : neither nor can be varied at all without losing a phase, pinning the triple point to a unique — the reason it is used as a fixed calibration reference for temperature scales.
Common traps
- Applying (valid for vaporisation/sublimation) to the fusion curve — both phases there are condensed, so is small and can even be negative, which is why ice's melting curve has a negative slope via .
- Confusing " degrees of freedom" with a count of phases or components — counts independently variable intensive variables like and , not how many substances or phases are present.
- Treating as truly constant over a wide temperature range in the integrated equation — it shrinks toward zero as 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 along a curve to the Clausius–Clapeyron slope formula felt rushed, ask the AI tutor to expand 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 corresponds to a lower temperature — so the same water boils at, say, instead of where the local atmospheric pressure matches roughly , 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 accounts for the two intensive variables, temperature and pressure, that describe a pure system before any phase-coexistence constraints are applied. Each additional phase in equilibrium imposes one more chemical-potential-equality constraint (), which removes one degree of freedom — hence subtracting . Composition variables would add further terms in a multi-component system, but for the 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 , 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 with the actual (small, sometimes negative) .