Boiling Point Calculator
Calculate boiling point at any external pressure using the Clausius-Clapeyron equation. Altitude correction (barometric formula), vacuum distillation BP, and normal BP from two vapour pressure measurements.
Find temperature where vapour pressure = target pressure
BP (normal) from two VP measurements at known temperatures
BP correction for altitude above sea level
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Calculate vapour pressure at any temperature using the Clausius-Clapeyron equation.
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Why use the LazyTools Boiling Point Calculator?
BP at any pressure
Clausius-Clapeyron rearranged to find T where VP = target P.
Altitude correction
Barometric formula (1 - h*2.26e-5)^5.256 for atmospheric P at any altitude.
Normal BP from two VP points
Two-point method gives delta-Hvap and normal BP simultaneously.
K and deg C both shown
Boiling point displayed in both Kelvin and Celsius.
Water, ethanol, methanol, acetone
Common solvents pre-loaded.
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How to use this tool in three steps
Select mode
BP at pressure, BP from two VP pairs, or altitude correction.
Enter reference boiling point and delta-Hvap
Or two vapour pressure measurements with temperatures.
Enter target pressure or altitude
kPa for pressure mode; metres for altitude mode.
Click Calculate
Boiling point in K and deg C shown.
LazyTools vs other Boiling Point Calculator tools
| Feature | LazyTools | Omnicalculator | NIST WebBook | Manual |
|---|---|---|---|---|
| BP at pressure | YES | ✓ Yes | ✓ Yes | ✓ Yes |
| Altitude correction | YES | ✗ No | ✗ No | ✓ Yes |
| BP from two VP | YES | ✗ No | ✗ No | ✓ Yes |
| Common solvents | YES | ✓ Yes | ✓ Yes | ✗ No |
| No signup | YES | ✓ Yes | ✗ No | ✓ Yes |
Boiling points of water at selected pressures and altitudes
| Pressure (kPa) | Altitude (m approx) | BP water (deg C) | BP ethanol (deg C) | Notes |
|---|---|---|---|---|
| 101.325 | 0 (sea level) | 100.0 | 78.4 | Normal BP |
| 89.9 | 1000 | 96.7 | 75.4 | Moderate altitude |
| 79.5 | 2000 | 93.2 | 72.2 | High altitude city |
| 70.1 | 3000 | 89.8 | 69.1 | Andean cities |
| 60.0 | 4000 | 85.9 | 65.5 | High mountain |
| 10.0 | vacuum | 45.8 | 34.2 | Vacuum distillation |
| 5.0 | deep vacuum | 32.9 | 23.7 | Rotary evaporator |
| 200 | pressure cooker | 120.2 | approx 95 | Pressure cooking |
Boiling Point Calculator: Complete Guide
A liquid boils when its vapour pressure equals the external pressure. The normal boiling point is defined at 1 atm (101.325 kPa). At lower pressures (reduced pressure distillation, altitude), the boiling point is lower; at higher pressures (pressure cookers, autoclaves), it is higher. The Clausius-Clapeyron equation: ln(P2/P1) = -(delta-Hvap/R) x (1/T2 - 1/T1) relates vapour pressure and temperature, allowing boiling point calculation at any pressure.
Boiling point at reduced pressure (vacuum distillation)
Vacuum distillation is used to purify thermally labile compounds at temperatures below their atmospheric boiling points. Example: a compound with normal BP 200 deg C and delta-Hvap = 45 kJ/mol. At 10 mbar (1.0 kPa): 1/T2 = 1/473.15 + (8.314/45000) x ln(1.0/101.325) = 2.114 x 10^-3 + 1.847 x 10^-4 x (-4.618) = 2.114 x 10^-3 - 8.53 x 10^-4 = 1.261 x 10^-3; T2 = 793 K -- that would be higher, which is wrong. Correctly: 1/T2 = 1/T1 + (R/dH)*ln(P2/P1). ln(1/101.325) = -4.618. 1/T2 = 2.114e-3 + 1.847e-4*(-4.618) = 2.114e-3 - 8.53e-4 = 1.261e-3. Wait: 2.114e-3 - 0.853e-3 = 1.261e-3. T2 = 793 K? That cannot be right. Let me recalculate: 1/473 = 0.002114; 8.314/45000 = 1.847e-4; 1.847e-4 * (-4.618) = -8.53e-4; sum = 2.114e-3 - 8.53e-4 = 1.261e-3; T2 = 1/1.261e-3 = 793. That is ~520 deg C, clearly wrong. The issue: at lower P, T should be lower. The Clausius-Clapeyron rearrangement: 1/T2 = 1/T1 - (R/dH)*ln(P2/P1). With P2 < P1, ln is negative, so we subtract a negative = add positive to 1/T1, giving 1/T2 > 1/T1, so T2 < T1. Recalculate: 1/T2 = 1/473.15 - (8.314/45000)*(-4.618) = 2.114e-3 + 8.53e-4 = 2.967e-3; T2 = 337 K = 64 deg C. This result makes sense -- vacuum distillation at 1 kPa reduces the BP from 200 to 64 deg C. The sign convention in the Clausius-Clapeyron equation must be carefully applied: this calculator uses the correct rearrangement.
Boiling point at altitude
Atmospheric pressure decreases with altitude: P = 101.325 x (1 - h x 2.2558 x 10^-5)^5.256 kPa (barometric formula, h in metres). At 1000 m: P = 101.325 x (1 - 2.2558 x 10^-2)^5.256 = 101.325 x 0.888 = 89.9 kPa. Water BP at 1000 m: approximately 96.7 deg C. At 3000 m (altitude of many Andean cities, e.g. Bogota 2640 m, Quito 2850 m): P approximately 70 kPa; water BP approximately 90 deg C. At 5895 m (Kilimanjaro summit): P approximately 49 kPa; water BP approximately 82 deg C. At 8849 m (Everest summit): P approximately 33 kPa; water BP approximately 72 deg C. The reduced boiling point has practical consequences: cooking times increase significantly at altitude (food cooks more slowly at lower temperature). Pasta takes approximately 25% longer at 2000 m; rice and vegetables are similarly affected. Pressure cookers restore near-sea-level conditions by increasing pressure inside the pot.
Boiling point in process chemistry
Organic chemists use boiling point data extensively for solvent selection, distillation design and reaction temperature control. A solvent boiling above 150 deg C at atmospheric pressure can be distilled cleanly at 10 to 20 mbar vacuum to give a BP below 50 deg C -- avoiding thermal decomposition. Rotary evaporators operate at 5 to 50 mbar and 25 to 40 deg C water bath temperature to remove common solvents (methanol BP 25 deg C at 6 kPa; acetone BP 22 deg C at 5 kPa; THF BP 28 deg C at 8 kPa; DMF BP 76 deg C at 8 kPa). The Dortmund Data Bank (DDB) and NIST WebBook are the primary sources of experimental vapour pressure data for process calculations.
Step-by-step worked example
A chemical engineer is designing a process to produce liquid ammonia from nitrogen and hydrogen gases at 25 deg C and 1 bar. The reaction is: N2(g) + 3H2(g) -> 2NH3(g). Standard thermodynamic data at 298 K: delta-Hf(NH3) = -46.11 kJ/mol; S(N2) = 191.6 J/mol/K; S(H2) = 130.7 J/mol/K; S(NH3) = 192.8 J/mol/K. Step 1 -- calculate delta-H: delta-H = 2 x (-46.11) - (0 + 3 x 0) = -92.22 kJ. Step 2 -- calculate delta-S: delta-S = 2 x 192.8 - (191.6 + 3 x 130.7) = 385.6 - (191.6 + 392.1) = 385.6 - 583.7 = -198.1 J/K = -0.1981 kJ/K. Step 3 -- calculate delta-G at 298 K: delta-G = delta-H - T x delta-S = -92.22 - 298 x (-0.1981) = -92.22 + 59.03 = -33.19 kJ. Step 4 -- check sign: delta-G < 0 -- reaction is spontaneous at 25 deg C. Step 5 -- calculate Kc: delta-G = -RT ln(K); K = exp(-delta-G/RT) = exp(33190/(8.314 x 298)) = exp(13.39) = 6.6 x 10^5. Very large K -- products strongly favoured thermodynamically. Step 6 -- note the kinetic problem: despite favourable thermodynamics (large K, negative delta-G), the reaction is kinetically very slow at 25 deg C. This is why the Haber process operates at 400 to 500 deg C with an iron catalyst -- kinetics are too slow at low temperature even though thermodynamics are more favourable there. At 500 deg C (773 K): delta-G = -92.22 - 773 x (-0.1981) = -92.22 + 153.1 = +60.88 kJ. Now delta-G > 0 and K = exp(-60880/(8.314 x 773)) = exp(-9.47) = 7.7 x 10^-5. K is small at high T -- only 15 to 25% conversion per pass. High pressure is used to compensate (shifts equilibrium toward fewer gas moles, increasing ammonia yield). This full analysis -- delta-H, delta-S, delta-G, K at two temperatures, and qualitative kinetic reasoning -- integrates the complete Chemical Thermodynamics suite.
Connections to the thermodynamics suite
The twelve Chemical Thermodynamics calculators in LazyTools cover every major thermodynamic calculation needed in chemistry and chemical engineering. The Gibbs Free Energy Calculator computes delta-G from delta-H and delta-S and predicts spontaneity. The Entropy Calculator sums standard molar entropies from NIST or textbook tables. The Equilibrium Constant Calculator connects K to delta-G via delta-G = -RT*ln(K). The Arrhenius Equation Calculator predicts k at any temperature from Ea and A, bridging thermodynamics and kinetics. The Vapor Pressure Calculator uses the Clausius-Clapeyron equation to find vapour pressure at any temperature from the enthalpy of vaporisation. The Boiling Point Calculator finds the normal boiling point from vapour pressure data. The Boiling Point Altitude Calculator adjusts boiling point for atmospheric pressure at altitude. The Boiling Point Elevation Calculator gives delta-Tb = i*Kb*m for solutions. The Freezing Point Depression Calculator gives delta-Tf = i*Kf*m. The STP Calculator converts between STP and SATP volumes. The Q10 Calculator gives the temperature sensitivity ratio for biochemical reactions. The Gibbs Phase Rule Calculator applies F = C - P + 2 to phase diagrams. Together these twelve calculators span reaction thermodynamics, phase equilibria and colligative properties -- the core quantitative content of undergraduate physical chemistry.
Thermodynamics in industry and environment
Chemical thermodynamics calculations are fundamental to engineering design. Delta-G determines whether a reaction is thermodynamically feasible under proposed conditions before any experimental work is done -- saving enormous amounts of laboratory time and resources. Process engineers use delta-H data to design heat exchangers (heat integration across exothermic and endothermic reaction stages). Entropy calculations guide understanding of process irreversibility and efficiency losses. The Clausius-Clapeyron equation is used in distillation column design (vapour pressure at every stage), in refrigeration system design (refrigerant properties), and in predicting the boiling point of mixtures. Colligative property calculations (boiling point elevation, freezing point depression) are used in antifreeze formulation, food preservation, pharmaceutical parenteral formulation (osmolarity of IV fluids), and polymer solution characterisation. The Gibbs phase rule constrains the number of independent variables in multi-component phase systems -- essential for alloy phase diagram interpretation, extraction process design, and supercritical fluid applications. All results in this suite display units and formulas explicitly, enabling straightforward verification and documentation for regulated engineering and pharmaceutical applications.
Worked numerical example
A chemical engineer is evaluating the feasibility of a new industrial process at 600 K. The proposed reaction is: CO2(g) + 4H2(g) -> CH4(g) + 2H2O(g) (Sabatier reaction for methane production from CO2 and green hydrogen). Standard thermodynamic data at 298 K: delta-Hf values -- CO2(g) -393.5, H2(g) 0, CH4(g) -74.8, H2O(g) -241.8 kJ/mol. Standard molar entropies -- CO2 213.8, H2 130.7, CH4 186.3, H2O(g) 188.8 J/mol/K. Step 1 -- calculate delta-H_rxn: delta-H = [(-74.8) + 2(-241.8)] - [(-393.5) + 4(0)] = (-74.8 - 483.6) - (-393.5) = -558.4 + 393.5 = -164.9 kJ. Exothermic. Step 2 -- calculate delta-S_rxn: delta-S = [186.3 + 2(188.8)] - [213.8 + 4(130.7)] = [186.3 + 377.6] - [213.8 + 522.8] = 563.9 - 736.6 = -172.7 J/K = -0.1727 kJ/K. Entropy decreases (5 mol gas -> 3 mol gas). Step 3 -- delta-G at 298 K: delta-G = -164.9 - 298(-0.1727) = -164.9 + 51.46 = -113.4 kJ. Spontaneous at 298 K; K = exp(113400/(8.314 x 298)) = exp(45.8) = 7.4 x 10^19. Very product-favoured thermodynamically. Step 4 -- delta-G at 600 K: delta-G = -164.9 - 600(-0.1727) = -164.9 + 103.6 = -61.3 kJ. Still spontaneous at 600 K, K = exp(61300/(8.314 x 600)) = exp(12.3) = 2.2 x 10^5. Still large but smaller -- lower temperature is thermodynamically preferred. Step 5 -- crossover temperature (delta-G = 0): T = delta-H/delta-S = -164900/(-172.7) = 955 K. Above 955 K the reaction becomes non-spontaneous. Process engineering conclusion: operate below 955 K with a catalyst (Ni or Ru) to achieve reasonable reaction rates. The Sabatier process is commercially operated at 300 to 400 deg C (573 to 673 K) with Ni catalyst, giving high conversion and good selectivity to methane.
Chemical thermodynamics in industrial and environmental contexts
Thermodynamic calculations of delta-G, delta-H and delta-S underpin every large-scale chemical process. Carbon capture and utilisation (CCU) processes like the Sabatier reaction and Fischer-Tropsch synthesis use thermodynamic feasibility calculations to screen reactions before committing to experimental and pilot plant work. The Haber-Bosch process (N2 + 3H2 -> 2NH3, delta-G = -33 kJ/mol at 298 K, delta-S = -198 J/K) operates below the thermodynamic crossover temperature of 467 K (194 deg C) to maintain negative delta-G, but uses elevated temperature (450 deg C) for acceptable kinetics -- at significant thermodynamic cost in equilibrium yield. Environmental chemistry uses Gibbs energy to predict which pollutants will persist in the environment (delta-G for aerobic degradation), whether metals will dissolve in groundwater (delta-G for dissolution vs precipitation), and whether greenhouse gases will react with atmospheric species (very negative delta-G values for OH radical reactions drive atmospheric chemistry). Biochemical thermodynamics: ATP hydrolysis (delta-G approximately -30 kJ/mol under cellular conditions) drives biosynthesis, active transport and mechanical work. Coupled reactions with negative delta-G drive unfavourable reactions with positive delta-G -- the universal biological energy currency.
Precision and limitations of thermodynamic calculations
Standard thermodynamic data (delta-Hf, S) are measured at 298 K and 1 bar. Using these values to predict delta-G at other temperatures involves two approximations: (1) delta-H is assumed constant with temperature (Kirchhoff's law: d(delta-H)/dT = delta-Cp, where delta-Cp is the heat capacity difference; for reactions without phase changes, delta-Cp is typically 5 to 50 J/mol/K, causing delta-H to change by 0.5 to 5 kJ per 100 K). (2) delta-S is assumed constant with temperature (similarly, d(delta-S)/dT = delta-Cp/T). For temperature extrapolation beyond 200 to 300 K from the reference temperature, these errors accumulate and more accurate calculations require integrating heat capacity data (Shomate equation or NASA polynomial fits). For engineering design, the JANAF tables (National Institute of Standards and Technology), HSC Chemistry software, and the Dortmund Data Bank provide temperature-dependent thermodynamic data. For regulatory submissions to the FDA or EMA for pharmaceutical manufacturing processes, thermodynamic calculations must be documented, justified, and accompanied by experimental validation at the intended process conditions. All calculations in this suite display the formula and inputs explicitly to enable straightforward documentation and verification.
Frequently asked questions
A liquid boils when its vapour pressure equals the external pressure. Higher external P = higher BP; lower P = lower BP.
Approximately 93 deg C (atmospheric P approximately 79.5 kPa at 2000 m).
Approximately 120 deg C, which significantly speeds up cooking.
Use Clausius-Clapeyron: 1/T2 = 1/T1 - (R/delta-Hvap)*ln(P2/P1). Enter normal BP and delta-Hvap.
To distil thermally sensitive compounds below their decomposition temperature by reducing the boiling point.
Approximately 7000 m, where atmospheric pressure is about 40 kPa.
P = 101.325 x (1 - h*2.2558e-5)^5.256 kPa, where h is altitude in metres.
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