🧊Phase Diagram Explorer - Water & CO₂ Phase Diagrams, Triple Point, Clausius–Clapeyron
Explore real pressure–temperature phase diagrams for water (IAPWS), carbon dioxide and nitrogen on a log pressure axis, and drag the state point to see its phase and the melting and boiling points at that pressure. Animated paths such as a pressure cooker, boiling water on Everest, freeze-drying, dry ice and supercritical CO₂ extraction list every phase change along the way. Further tabs cover Clausius–Clapeyron, boiling points by altitude or cooker gauge pressure, and van der Waals isotherms for CO₂ with the Maxwell construction.
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How to use Phase diagrams & phase transitions
- 1Choose water, carbon dioxide or nitrogen, or define your own substance from its triple point, critical point, heat of fusion and volume change
- 2Press and drag the state point to read the phase, degrees of freedom and the melting, boiling or sublimation point at that pressure
- 3Pick a process path and play it to watch melting, boiling, sublimation or a continuous trip around the critical point
- 4Use the other tabs to get latent heat from two points, boiling points at altitude or in a pressure cooker, and van der Waals isotherms
FAQ
- Why does water's melting line lean to the left?
- The Clapeyron equation gives dP/dT = ΔH/(TΔV). Ice is less dense than water, so melting shrinks the volume (ΔV ≈ −1.63 cm³/mol) and the slope is negative, about −13.5 MPa/K. Pressure therefore lowers the melting point. Most substances, including CO₂ and N₂, have a denser solid and a positive slope. The line is very steep, though: lowering the melting point of ice by 1 °C takes about 133 atmospheres.
- Why doesn't dry ice melt into a liquid?
- The triple-point pressure of CO₂ is 5.18 atm (518 kPa), and liquid CO₂ cannot exist below it. Heating dry ice at 1 atm moves the state point across the sublimation curve, so it turns straight into gas at −78.5 °C (194.7 K). To get liquid CO₂ you need more than 5.18 atm, such as the roughly 6 MPa inside a cylinder at room temperature.
- How hot is the water in a pressure cooker?
- The absolute pressure inside is local air pressure plus the gauge reading. At a typical 100 kPa gauge the absolute pressure is about 201 kPa and water boils at about 120 °C; at 50 kPa gauge it is about 111 °C. At high altitude the air pressure is lower, so the same gauge pressure gives a lower boiling point, and the calculator here accounts for altitude.
- What is a supercritical fluid?
- Above both the critical temperature and pressure (374 °C and 22.06 MPa for water, 31 °C and 7.38 MPa for CO₂), liquid and gas have the same density and there is no boiling interface. The result is a supercritical fluid: it diffuses like a gas and dissolves things like a liquid, which is why supercritical CO₂ is used to decaffeinate coffee and extract flavors. By going around the critical point, a gas can turn into a liquid without ever boiling.
- Why does the van der Waals isotherm have a loop?
- Below the critical temperature, a vdW isotherm has a stretch where dP/dV > 0. That part is mechanically unstable, so a real fluid splits into liquid and vapor at the saturation pressure. The Maxwell equal-area rule places this horizontal line so the areas enclosed above and below it are equal. The vdW equation gets the critical point and coexistence right qualitatively, but not quantitatively: for CO₂ at 280 K it predicts 5.3 MPa versus about 4.2 MPa in reality.
Features
- Accurate phase boundaries: IAPWS vapor pressure, sublimation and ice Ih–VII melting curves; Span–Wagner for CO₂ and N₂
- Draggable state point with phase, Gibbs phase rule degrees of freedom and vapor pressure
- Eight animated process paths with every transition located automatically
- Clausius–Clapeyron in three modes compared with IAPWS data, plus the Clapeyron melting-line slope
- Boiling point from altitude or pressure, and pressure cooker temperature from gauge pressure
- Van der Waals isotherms for CO₂ with Maxwell construction and the two-phase dome
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