Phase Diagram Calculator
Interactive P-T phase diagram for water with IAPWS saturation, sublimation and melting curves, triple and critical points, region lookup and process path plotting
Interactive pressure-temperature phase diagram for water. Hover to see properties. Shows the saturation curve (IAPWS-IF97) from the triple point (0.01°C, 611.657 Pa) to the critical point (373.946°C, 22.064 MPa), and the sublimation and melting curves of ice from IAPWS R14-08.
Water P-T Phase Diagram
Saturation, Sublimation & Melting Curve Data Table
| Curve | T (°C) | P (MPa) |
|---|---|---|
| Sublimation | -50.00 | 3.9377e-6 |
| Sublimation | -47.50 | 5.3436e-6 |
| Sublimation | -45.00 | 7.2032e-6 |
| Sublimation | -42.50 | 9.6477e-6 |
| Sublimation | -40.00 | 1.2841e-5 |
| Sublimation | -37.50 | 1.6989e-5 |
| Sublimation | -35.00 | 2.2344e-5 |
| Sublimation | -32.50 | 2.9221e-5 |
| Sublimation | -30.00 | 3.8005e-5 |
| Sublimation | -27.50 | 4.9165e-5 |
| Sublimation | -25.00 | 6.3274e-5 |
| Sublimation | -22.50 | 8.1021e-5 |
| Sublimation | -20.00 | 1.0324e-4 |
| Sublimation | -17.50 | 1.3093e-4 |
| Sublimation | -15.00 | 1.6527e-4 |
| Sublimation | -12.50 | 2.0770e-4 |
| Sublimation | -10.00 | 2.5987e-4 |
| Sublimation | -7.50 | 3.2378e-4 |
| Sublimation | -5.00 | 4.0174e-4 |
| Sublimation | -2.50 | 4.9647e-4 |
| Sublimation | 0.01 | 6.1166e-4 |
| Melting (ice Ih) | 0.01000 | 0.000611657 |
| Melting (ice Ih) | 0.00999 | 0.000746313 |
| Melting (ice Ih) | 0.00990 | 0.00195821 |
| Melting (ice Ih) | 0.00900 | 0.0140769 |
| Melting (ice Ih) | 0.00700 | 0.0410049 |
| Melting (ice Ih) | 0.00000 | 0.135229 |
| Melting (ice Ih) | -0.02000 | 0.404232 |
| Melting (ice Ih) | -0.09000 | 1.34333 |
| Melting (ice Ih) | -0.29000 | 4.00615 |
| Melting (ice Ih) | -0.99000 | 13.1024 |
| Melting (ice Ih) | -1.99000 | 25.5552 |
| Melting (ice Ih) | -3.99000 | 48.8759 |
| Melting (ice Ih) | -5.99000 | 70.4996 |
| Melting (ice Ih) | -7.99000 | 90.7665 |
| Melting (ice Ih) | -9.99000 | 109.910 |
| Melting (ice Ih) | -11.99000 | 128.101 |
| Melting (ice Ih) | -13.99000 | 145.471 |
| Melting (ice Ih) | -15.99000 | 162.128 |
| Melting (ice Ih) | -17.99000 | 178.156 |
| Melting (ice Ih) | -19.99000 | 193.628 |
| Melting (ice Ih) | -21.98500 | 208.567 |
| Melting (ice III) | -21.98500 | 208.566 |
| Melting (ice III) | -20.98500 | 225.409 |
| Melting (ice III) | -19.98500 | 246.691 |
| Melting (ice III) | -18.98500 | 273.559 |
| Melting (ice III) | -17.98500 | 307.446 |
| Melting (ice III) | -16.98600 | 350.100 |
| Melting (ice V) | -16.98600 | 350.100 |
| Melting (ice V) | -14.98600 | 376.782 |
| Melting (ice V) | -12.98600 | 404.950 |
| Melting (ice V) | -10.98600 | 434.676 |
| Melting (ice V) | -8.98600 | 466.032 |
| Melting (ice V) | -6.98600 | 499.095 |
| Melting (ice V) | -4.98600 | 533.943 |
| Melting (ice V) | -2.98600 | 570.659 |
| Melting (ice V) | -0.98600 | 609.328 |
| Melting (ice V) | 0.16000 | 632.399 |
| Melting (ice VI) | 0.16000 | 632.400 |
| Melting (ice VI) | 2.16000 | 655.582 |
| Melting (ice VI) | 4.16000 | 679.379 |
| Melting (ice VI) | 6.16000 | 703.801 |
| Melting (ice VI) | 8.16000 | 728.861 |
| Melting (ice VI) | 10.16000 | 754.571 |
| Melting (ice VI) | 12.16000 | 780.943 |
| Melting (ice VI) | 14.16000 | 807.988 |
| Melting (ice VI) | 16.16000 | 835.720 |
| Melting (ice VI) | 18.16000 | 864.151 |
| Melting (ice VI) | 20.16000 | 893.293 |
| Melting (ice VI) | 22.16000 | 923.159 |
| Melting (ice VI) | 24.16000 | 953.762 |
| Melting (ice VI) | 26.16000 | 985.116 |
| Saturation | 0.01 | 0.000612 |
| Saturation | 5.00 | 0.000873 |
| Saturation | 10.00 | 0.001228 |
| Saturation | 20.00 | 0.002339 |
| Saturation | 30.00 | 0.004247 |
| Saturation | 40.00 | 0.007384 |
| Saturation | 50.00 | 0.012351 |
| Saturation | 60.00 | 0.019946 |
| Saturation | 70.00 | 0.031201 |
| Saturation | 80.00 | 0.047415 |
| Saturation | 90.00 | 0.070182 |
| Saturation | 100.00 | 0.101418 |
| Saturation | 110.00 | 0.143376 |
| Saturation | 120.00 | 0.198665 |
| Saturation | 130.00 | 0.270260 |
| Saturation | 140.00 | 0.361501 |
| Saturation | 150.00 | 0.476101 |
| Saturation | 160.00 | 0.618139 |
| Saturation | 170.00 | 0.792053 |
| Saturation | 180.00 | 1.002635 |
| Saturation | 190.00 | 1.255018 |
| Saturation | 200.00 | 1.554672 |
| Saturation | 210.00 | 1.907391 |
| Saturation | 220.00 | 2.319288 |
| Saturation | 230.00 | 2.796792 |
| Saturation | 240.00 | 3.346652 |
| Saturation | 250.00 | 3.975939 |
| Saturation | 260.00 | 4.692071 |
| Saturation | 270.00 | 5.502839 |
| Saturation | 280.00 | 6.416459 |
| Saturation | 290.00 | 7.441643 |
| Saturation | 300.00 | 8.587708 |
| Saturation | 310.00 | 9.864746 |
| Saturation | 320.00 | 11.283856 |
| Saturation | 330.00 | 12.857522 |
| Saturation | 340.00 | 14.600181 |
| Saturation | 350.00 | 16.529164 |
| Saturation | 360.00 | 18.666403 |
| Saturation | 370.00 | 21.043367 |
| Saturation | 373.95 | 22.064000 |
Look Up Point
Compressed Liquid
Above the saturation pressure at 150 °C: 0.4761 MPa.
Plot Process Path (optional)
Reference points
Triple Point: T = 0.01°C, P = 0.000611657 MPa (611.657 Pa). Ice, liquid water and vapor coexist.
Critical Point: T = 373.946°C, P = 22.064 MPa. Liquid and vapor become indistinguishable.
Normal Boiling Point: T = 99.974°C at P = 0.101325 MPa (1 atm), from IAPWS-IF97 (100°C on the older IPTS-68 temperature scale).
Regions: Below the saturation and sublimation curves is vapor (gas). Above the saturation curve and to the right of the melting curve is liquid; left of the melting and sublimation curves is ice. Above the critical temperature and pressure is supercritical fluid.
Sources: saturation pressure from IAPWS-IF97 (IAPWS R7-97(2012)); sublimation and melting pressures from IAPWS R14-08(2011). R14-08 gives no boundaries between the ice phases, so points in the solid region are labelled "Solid (Ice)" without naming the ice form.
How to Use This Calculator
Enter your input values
Fill in all required input fields for the Phase Diagram Calculator. Follow the units and input format printed next to each field. Where a unit selector is available, choose the units that match your data.
Review your inputs
Double-check that all values are correct and match the units or format shown for each field. Incorrect units are the most common source of calculation errors and can produce results that are off by factors of 2, 10, or more.
Read the results
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Explore parameter sensitivity
Try adjusting individual input values to see how the output changes. This is a quick and effective way to develop intuition about how different parameters influence the result and to identify which inputs have the largest effect.
When to Use This Calculator
- •Use the Phase Diagram Calculator to check your hand calculations on homework or exam problems — comparing its result with your own working helps identify arithmetic errors before they propagate.
- •Use it during the early design phase to rapidly iterate on parameters and narrow down feasible configurations before committing time to detailed finite element simulations or full design packages.
- •Use it when reviewing a colleague's calculation or checking a vendor's data sheet for plausibility — a quick sanity check can prevent costly downstream errors.
- •Use it to generate reference data for a technical report or presentation without manual computation, ensuring consistent, reproducible numbers throughout the document.
- •Use it in the field when a quick estimate is needed and a full engineering software package is not available.
About This Calculator
The Phase Diagram Calculator is a precision engineering calculation tool designed for students, engineers, and technical professionals. Interactive P-T phase diagram for water with IAPWS saturation, sublimation and melting curves, triple and critical points, region lookup and process path plotting All calculations are performed using established engineering formulas from the relevant scientific literature and standards. Follow the units printed beside each field. Where a unit selector is provided, the selected unit is converted internally. Results are computed in your browser without sending data to a server, which keeps your inputs private. This calculator is intended as a supplementary tool for learning and design exploration; always verify results against authoritative references for safety-critical applications.
The Theory Behind It
A phase diagram for a pure substance shows the stable phase (solid, liquid, vapor, supercritical) as a function of two independent variables, most commonly pressure and temperature. The key features on a P-T diagram are: the sublimation line (solid-vapor coexistence at low pressures), the melting line (solid-liquid coexistence, nearly vertical because solid and liquid have similar specific volumes, so the Clapeyron slope dP/dT = Δs/Δv is steep), the vaporization line or saturation curve (liquid-vapor coexistence, curving upward from the triple point to the critical point), the triple point (where all three phases coexist, a unique P and T for each substance), and the critical point (the end of the liquid-vapor coexistence line, above which the substance is 'supercritical' with continuous density variation between liquid-like and vapor-like). Water has an unusual negative slope to its ice Ih melting line: increasing pressure lowers the melting point, by about 0.074 K per MPa near 0 °C (the IAPWS melting curve rises about 13.5 MPa per kelvin of cooling). That is far too little for the few megapascals under a skate blade to melt ice at −10 °C; frictional heating and a thin premelted surface layer are the accepted explanations of why ice is slippery. Most other substances have positive melting lines. The critical point for water is T_c = 373.95°C and P_c = 22.064 MPa. The triple point of water (where ice, liquid, and vapor coexist) is T = 0.01°C and P = 611.657 Pa, which has been used as a temperature reference. Above the critical temperature, water is a supercritical fluid with no distinct phase boundaries — industrially important for supercritical power plants (efficient steam cycles above the critical pressure) and for chemistry (supercritical water oxidation for waste treatment, supercritical CO₂ for extraction). The calculator draws the saturation curve from IAPWS-IF97 and the sublimation and ice Ih, III, V and VI melting curves from IAPWS R14-08, and classifies any (P, T) point against those same curves.
Real-World Applications
- •Cooking at high altitude: at lower atmospheric pressure (higher altitude), water boils at lower temperature. At 3000 m elevation, where the standard-atmosphere pressure is about 70 kPa, water boils at about 90°C — which changes cooking times significantly. Phase diagrams explain this effect directly.
- •Freeze drying (lyophilization): food and pharmaceutical preservation uses low-pressure sublimation. Ice is converted directly to vapor without passing through the liquid phase, avoiding heat damage. Operating at 0.1 kPa keeps water in the solid-vapor regime.
- •Supercritical CO₂ extraction: industrial-scale extraction of caffeine, essential oils, and other compounds uses supercritical CO₂ (T > 31°C, P > 7.4 MPa). The supercritical fluid penetrates like a gas but dissolves like a liquid.
- •High-pressure ice and liquid: below 0 °C water stays liquid only above the ice Ih melting pressure (about 60 MPa at −5 °C), and below 0 °C remains liquid between the ice Ih melting pressure and the melting pressure of a denser ice. That upper limit rises from about 209 MPa at −22 °C (the Ih–III–liquid triple point) to about 632 MPa at 0.16 °C (the V–VI–liquid triple point); the upper limit is about 534 MPa at −5 °C. These are the temperature-dependent boundaries drawn from IAPWS R14-08.
- •Rankine cycle design: boiler and condenser pressures must be chosen to place the cycle within safe operating regions on the phase diagram. Below the triple-point pressure liquid water cannot exist, and above the critical pressure the boiler has no boiling plateau (a supercritical cycle).
Frequently Asked Questions
What's a phase diagram?
A phase diagram shows the thermodynamic phase (solid, liquid, vapor, or supercritical) as a function of two state variables, usually pressure and temperature. Boundaries between phases indicate coexistence conditions (where two phases are in equilibrium). Key points: triple point (three phases coexist), critical point (end of liquid-vapor coexistence), melting line (solid-liquid boundary), and vaporization line (liquid-vapor boundary).
What's special about water's phase diagram?
Water's melting line has a NEGATIVE slope (dT/dP < 0), meaning the melting point DECREASES with increasing pressure. This is unusual — most substances have positive-slope melting lines. The negative slope arises because ice is LESS dense than liquid water (unlike most solids being denser than their liquids), so compressing ice favors liquid phase. This is why ice floats in water, why pressure lowers the melting point (slightly: about 0.074 K per MPa near 0 °C), and why frozen pipes burst.
What's the critical point?
The critical point is the temperature and pressure above which the liquid-vapor distinction disappears. For water: T_c = 373.95°C and P_c = 22.064 MPa. Above the critical temperature, no amount of pressure can liquefy the gas. Above the critical pressure, the substance smoothly changes from liquid-like to gas-like as temperature increases, without a phase transition. Supercritical fluids have properties intermediate between liquid and gas and are used in industrial extraction, supercritical power plants, and advanced oxidation processes.
What's the triple point?
The triple point is where all three phases (solid, liquid, vapor) coexist in equilibrium. It is a unique combination of temperature and pressure for each substance. For water: T = 0.01°C and P = 611.657 Pa. The triple point of water was historically used as a temperature reference in the Kelvin scale; the modern definition has moved to the Boltzmann constant, but the water triple point remains an important fixed point for calibration and metrology.
What happens below the triple point pressure?
Below the triple point pressure, liquid phase cannot exist — only solid and vapor, separated by a sublimation line. A block of ice at P < 611 Pa exposed to space would sublimate directly to vapor without melting. This is the basis of freeze drying (sublimation under vacuum for low-temperature dehydration) and explains why comets and asteroids in space show sublimation rather than melting when approaching the sun.
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References & Further Reading
Standards & Organizations
- IAPWS R7-97(2012): Revised Release on the IAPWS Industrial Formulation 1997 for the Thermodynamic Properties of Water and SteamIAPWS
The saturation curve.
- IAPWS R14-08(2011): Revised Release on the Pressure along the Melting and Sublimation Curves of Ordinary Water SubstanceIAPWS
The sublimation and melting curves this diagram draws.
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