Boiling Point Calculator
ChemistryCalculate the boiling point of a pure liquid or solution using the Clausius-Clapeyron equation or boiling point elevation formula. Supports water, ethanol, and more.
Boiling Point (°C)
What is a Boiling Point?
The Boiling Point Calculator computes the boiling point of a pure liquid (water, ethanol, methanol, acetone, or a custom liquid) at any atmospheric pressure using the Clausius-Clapeyron equation. Enter the pressure in mmHg and select the substance to instantly get the boiling temperature in °C, K, and °F.
The boiling point is the temperature at which a liquid's vapour pressure equals the surrounding external pressure. Since vapour pressure is a function of temperature (it increases exponentially with temperature), reducing the external pressure reduces the temperature at which boiling occurs. At 1 atm (760 mmHg), water boils at 100°C; at half that pressure (380 mmHg, approximately 5,500 m altitude), it boils at about 81°C.
This pressure-dependence is described by the Clausius-Clapeyron equation, which requires only the normal boiling point (at 760 mmHg) and the enthalpy of vaporisation (ΔHvap) to predict the boiling point at any other pressure. The calculator uses established ΔHvap values for each preset substance and applies the equation with automatic unit handling. For the Vapor Pressure Calculator, which solves the inverse problem (finding vapour pressure at a given temperature), see the related tool.
How to use this Boiling Point calculator
- Select the liquid from the Substance dropdown: Water, Ethanol, Methanol, Acetone, or Custom.
- Enter the operating pressure in mmHg in the Pressure field. Standard atmospheric pressure at sea level is 760 mmHg. Adjust lower for altitude or vacuum conditions, higher for pressurised systems.
- If using Custom, enter the normal boiling point in °C in the Normal Boiling Point field and the enthalpy of vaporisation in kJ/mol in the ΔHvap field.
- Read the Boiling Point (°C) — compare to the normal boiling point to understand the pressure effect.
- For cooking at altitude, use the result to estimate required extra cooking time (food cooks slower below 100°C) and whether a pressure cooker is needed.
Formula & Methodology
Clausius-Clapeyron equation (solved for T₂):ln(P₂/P₁) = (ΔHvap/R) × (1/T₁ − 1/T₂) 1/T₂ = 1/T₁ − (R/ΔHvap) × ln(P₂/P₁) T₂ = 1 / [1/T₁ − (R/ΔHvap) × ln(P₂/P₁)]Where: T₁ = normal boiling point (K, at P₁ = 760 mmHg), T₂ = boiling point at P₂, ΔHvap in J/mol (× 1000 from kJ/mol), R = 8.314 J/(mol·K) Worked example — water at Shimla altitude (≈ 640 mmHg): ΔHvap(water) = 40,700 J/mol, T₁ = 373.15 K (100°C), P₁ = 760 mmHg, P₂ = 640 mmHg1/T₂ = 1/373.15 − (8.314/40700) × ln(640/760) = 0.002680 − 0.0002043 × (−0.1719) = 0.002680 + 0.0000351 = 0.002715 T₂ = 1/0.002715 = 368.3 K = 95.2°CAt Shimla's altitude, water boils at approximately 95°C — explaining why rice and pulses take 15–20% longer to cook without a pressure cooker compared to sea-level cooking.
Frequently Asked Questions