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WaterVaporPressure

Water Phase Diagram

An interactive pressure–temperature map of water’s phases. The vaporization and sublimation curves are computed live from the IAPWS-95 and Murphy–Koop equations; move the marker to read the saturation pressure at any temperature.

1 Pa10 Pa100 Pa1 kPa10 kPa100 kPa1 MPa10 MPa100 MPa-60°C0°C100°C200°C300°C400°CTemperaturePressure (log scale)Solid (ice)LiquidVaporSupercriticaltriple pointcritical point
Vaporization (liquid ⇌ vapor)Sublimation (solid ⇌ vapor)Melting (schematic)

At 100 °C, the saturation pressure is 101.42 kPa. This is the boiling/condensation point, where liquid water and vapor coexist.

Reading the diagram

Each line is a coexistence boundary. The blue vaporization curve is exactly the saturation vapor pressure of water — the same quantity the main calculator returns — running from the triple point up to the critical point, where it ends. Below freezing, the cyan sublimation curve gives the frost point, where ice turns directly to vapor. The steep dashed melting curve divides ice from liquid water.

Pick any point in the plane and the phase is whichever region it falls in. On a boundary, two phases coexist — which is why water boils at 100 °C only at about one atmosphere, and at a lower temperature on a mountaintop where the pressure is lower. The marker traces that boiling (or frost) point as you change the temperature.

Frequently asked questions

What does the water phase diagram show?

It maps which phase of water — solid, liquid, or vapor — is stable at each combination of temperature and pressure. The lines are the boundaries where two phases coexist: the vaporization curve (liquid ⇌ vapor) is the saturation vapor pressure curve, the sublimation curve (solid ⇌ vapor) lies below freezing, and the steep melting curve (solid ⇌ liquid) separates ice from liquid water. Pressure is drawn on a logarithmic scale because it spans more than five orders of magnitude.

What are the triple point and critical point?

The triple point (0.01 °C, 611.657 Pa) is the single temperature and pressure at which solid, liquid, and vapor all coexist — it is the fixed point that anchors the temperature scale. The critical point (373.946 °C, 22.064 MPa) is where the liquid–vapor boundary ends: above it, liquid and vapor become indistinguishable and water is a supercritical fluid.

Why does the melting line of water tilt to the left?

Almost uniquely, water's solid–liquid boundary has a slightly negative slope: ice is less dense than liquid water, so increasing the pressure lowers the melting temperature. The effect is small (about −13.5 MPa per kelvin), so the line is nearly vertical; on this diagram it is drawn schematically.

Where do the curves come from?

The vaporization curve is computed from the IAPWS-95 saturation equation, the international reference standard, and the sublimation curve from the Murphy–Koop (2005) equation over ice — the same verified engine used across this site. The melting line is schematic. Move the temperature marker to read the exact saturation pressure at any point.

References

Every formula on this page is implemented from, and validated against, the following primary standards and papers.

Reviewed by Jimmy Raymond, Engineer
B.S. Environmental Engineering · B.S. Computer Science · Last reviewed June 4, 2026

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