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Chemistry

Boiling Point Calculator: Chemistry and Elevation

Updated · Standard formula, shown below

The calculator for this page is switched off while it is checked. The formula is below, and the worked example in the article shows how to use it by hand.

Boiling Point Calculator: Chemistry and Elevation

A boiling point calculator in chemistry estimates a liquid’s boiling point from its normal boiling point and the surrounding pressure, or estimates how a dissolved nonvolatile solute raises a solvent’s boiling point. Enter the measurements and the relevant substance data to get a temperature estimate; the calculation method depends on which effect you want to examine.

Formula

This calculator estimates a pure liquid’s boiling point at a pressure other than standard atmospheric pressure using a simplified Clausius–Clapeyron relation:

T₂ ≈ T₁ + (R T₁² / ΔHᵥₐₚ) ln(P₂ / P₁)

  • T₁ is the liquid’s normal boiling point in kelvins, where its vapor pressure equals standard pressure.
  • T₂ is the estimated boiling temperature in kelvins.
  • P₁ is the reference pressure, here 101.325 kPa.
  • P₂ is the surrounding pressure in kPa. It must be greater than zero.
  • R is the gas constant, 8.314 J mol⁻¹ K⁻¹.
  • ΔHᵥₐₚ is the molar enthalpy of vaporization in J/mol. The calculator’s coefficient assumes an approximate value of 40,700 J/mol, appropriate only as a rough illustration near water’s normal boiling point.

The coefficient 0.0487 in the calculator is the rounded value of R divided by that assumed enthalpy, expressed in kelvins per mole cancellation; the expression applies the correction in degrees Celsius, which have the same temperature interval size as kelvins. Because the calculation holds vaporization enthalpy constant, it is an approximation, not a substitute for experimental vapor-pressure data or a substance-specific equation.

Worked Example

Using the calculator’s defaults, the normal boiling point is 100 °C and pressure is 101.325 kPa. At the reference pressure, the logarithm of the pressure ratio is zero:

ln(101.325 / 101.325) = ln(1) = 0

So the estimated temperature is 100 + (100 + 273.15) × 0 × 0.0487 = 100.00 °C. In kelvins, that is 100.00 + 273.15 = 373.15 K. The result matches the reference boiling point because no pressure change was entered.

What a Boiling Point Means

A liquid boils when its vapor pressure equals the pressure exerted on its surface. Vapor pressure rises as temperature rises; when it reaches the surrounding pressure, vapor bubbles can form throughout the liquid, rather than only at its surface. The boiling point therefore is not an unchanging property independent of conditions.

Chemistry tables usually list a normal boiling point, meaning the boiling temperature at one standard atmosphere, 101.325 kPa (101,325 Pa, or 760 mmHg). For water this is 100 °C (212 °F) at that pressure. “Boiling point” without a stated pressure can be ambiguous, especially when comparing measurements made at different elevations or in laboratory apparatus.

Using the Pressure Estimate

Use the pressure method when you know a substance’s normal boiling point and want a first approximation for a different pressure. Pressure must be absolute pressure—not gauge pressure, which is measured relative to local atmospheric pressure. For instance, a gauge reading of zero does not mean zero absolute pressure; it means the pressure is approximately the local atmosphere.

  • At lower pressure, the pressure ratio is below one, its natural logarithm is negative, and the estimated boiling point falls.
  • At higher pressure, the ratio is above one and the estimate rises.
  • Use matching units for both pressures. The calculator accepts kPa; convert other values before entering them. One atmosphere is 101.325 kPa, and 1 bar is 100 kPa.
  • Enter the normal boiling point in degrees Celsius. The calculation converts it to an absolute temperature internally; Celsius and kelvin have equal-sized increments, but their zero points differ.

The simplified estimate works best for modest pressure changes near the reference boiling point. For large pressure changes, mixtures, or precise process work, use reliable vapor-pressure data or a more complete thermodynamic model. Enthalpy of vaporization changes with temperature, and real substances do not follow the constant-enthalpy approximation perfectly.

Boiling Point Elevation in Solutions

A different kind of boiling point calculator addresses boiling point elevation: the increase in a solvent’s boiling temperature after a nonvolatile solute is dissolved in it. The dilute-solution equation is ΔTᵦ = i Kᵦ m, where ΔTᵦ is the increase in kelvins or degrees Celsius, i is the van ’t Hoff factor (the effective number of dissolved particles per formula unit), Kᵦ is the solvent’s ebullioscopic constant in K·kg/mol, and m is solute molality in mol/kg of solvent.

Molality is moles of solute divided by kilograms of solvent, not kilograms of solution. For water, Kᵦ is approximately 0.512 K·kg/mol. If a dilute solution has an effective particle factor of 2 and molality 0.10 mol/kg, the estimated elevation is 2 × 0.512 × 0.10 = 0.1024 °C. The solution’s boiling point is therefore about 0.10 °C above that of the pure solvent at the same pressure. This example illustrates the formula; real solutions may deviate because particles interact or dissociate incompletely.

Pressure and solute effects are distinct. A salt solution can boil above pure water at the same pressure, while a liquid at high elevation boils at a lower temperature because atmospheric pressure is lower. To predict a real solution accurately, account for both pressure and composition with appropriate data; do not simply apply one formula outside its assumptions.

Common Errors and Limits

  • Confusing temperature scales: use kelvins for thermodynamic equations that require absolute temperature. A change of 1 K equals a change of 1 °C, but 0 K is not 0 °C.
  • Using gauge pressure: convert to absolute pressure by adding local atmospheric pressure when appropriate. A pressure ratio cannot use zero or negative absolute pressure.
  • Mixing pressure units: convert both pressures to the same units before forming a ratio.
  • Treating the estimate as exact: the calculator assumes a fixed vaporization enthalpy and is most defensible near its reference conditions. It does not account for impurities, decomposition, or chemical reactions.
  • Confusing boiling with evaporation: evaporation can occur below the boiling point; boiling requires the vapor pressure to reach the external pressure.

For exact laboratory reporting, specify the substance, purity, pressure, temperature scale, and measurement method. A calculator is useful for checking trends and obtaining a rough estimate, but precise boiling temperatures should come from dependable substance-specific measurements or validated data.

Frequently Asked Questions

Does a boiling point change with altitude?
Usually, yes. Atmospheric pressure generally decreases as altitude increases, so a liquid reaches the surrounding pressure at a lower temperature. Local weather and exact elevation affect the actual pressure.

Why does water boil below 100 °C in the mountains?
At higher elevations, the lower atmospheric pressure means water’s vapor pressure matches the surroundings at a lower temperature. The value 100 °C applies to water at 101.325 kPa, not every location.

Does adding salt raise water’s boiling point?
Yes, dissolved nonvolatile salt raises water’s boiling point, but ordinary cooking amounts produce a relatively small change. The size depends on the amount dissolved and the effective number of particles in solution.

Is boiling point the same as melting point?
No. Melting point is where solid and liquid phases are in equilibrium; boiling point is where a liquid’s vapor pressure equals its surrounding pressure. Both can depend on pressure, but they describe different phase changes.

Can this estimate be used for any chemical?
Not reliably as a precise result. The pressure estimate uses a simplified, water-like vaporization enthalpy assumption. For another chemical, use its own vapor-pressure data or enthalpy and an appropriate model.

Related

Formula used
in bp | Normal boiling point | °C | 100 | 
in p | Surrounding pressure | kPa | 101.325 | 0
out temp | Estimated boiling point | °C | (bp + 273.15) * ln(p / 101.325) * 0.0487 + bp | 2
out kelvin | Estimated boiling point | K | temp + 273.15 | 2

Each line is one input (in, sel, list) or one result (out: label, unit, formula, decimals). How the calculators work

Method: the standard formula for this calculation, rounded as each result states. See how the calculators work or report an error.