Temperature

Water triple point

The water triple point is the unique temperature and pressure at which water can exist simultaneously as solid, liquid, and vapour in equilibrium.

Also known as: triple point of water

How big is it?

0.01 °C

Also 32.02 °F

Triple-point temperature · specified

Scale illustration of Water triple point, calibrated to its triple-point temperature measurement.
The marked triple-point temperature represents 0.01 °C.

A little perspective

Water triple point is 29.75 K cooler than Gallium melting plateau at standard pressure.

Gallium melting plateau at standard pressure: This is the temperature at which pure gallium changes from solid to liquid under normal atmospheric pressure.

Kelvin scale
THERMODYNAMIC TEMPERATURE · KELVIN0.01 °C29.76 °C0 K · absolute zero
01
Water triple point0.01 °CTriple-point temperature
02
Gallium melting plateau at standard pressure29.76 °CEquilibrium melting temperature near 101 kPa
Celsius and Fahrenheit zero points are offsets. Compare temperature differences, not ratios in °C or °F. The kelvin axis starts at absolute zero.
Measurements, assumptions & sources +

Water triple point

The triple point of water is 273.16 K for a specified isotopic composition at its equilibrium pressure. It is distinct from ordinary freezing water at atmospheric pressure.

IAPWS — Fundamental physical constants of water

The marked triple-point temperature is calibrated. Unmeasured illustration details are representative.

Gallium melting plateau at standard pressure

Gallium melts at about 302.9146 K (29.7646 °C) near standard pressure. Purity and pressure affect a realised plateau.

NIST — ITS-90 fixed points

The marked equilibrium melting temperature near 101 kpa is calibrated. Unmeasured illustration details are representative.

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Why this measurement?

Why we use 0.01 °C

For comparison, this page uses triple-point temperature. The record labels this value specified, so the stated convention rather than an inferred average controls the comparison.

The triple point of water is 273.16 K for a specified isotopic composition at its equilibrium pressure. It is distinct from ordinary freezing water at atmospheric pressure.

The identifying illustration and the numerical comparison remain separate. How calibrated comparisons work →

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Recorded properties

Water triple point dimensions and measurements

PropertySelected valueRecorded rangeBasis
0.01 °CNot recordedspecified

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Sources and method

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