Dissolving anything in a liquid raises its boiling point — a small but measurable effect called boiling point elevation. It's one of four colligative properties, meaning it depends only on how many particles are dissolved, not on what they are. This calculator applies the standard formula ΔTb = i·Kb·m to find the elevation and the resulting boiling point for any solute-solvent combination.
How the formula works
Adding solute particles to a solvent lowers the solvent's vapor pressure at any given temperature, because solute particles occupy some of the surface where solvent molecules would otherwise escape into vapor. A liquid boils when its vapor pressure equals the surrounding atmospheric pressure, so a solution with lower vapor pressure needs a higher temperature to reach that same threshold — hence the elevation.
The relationship ΔTb = i·Kb·m captures this exactly: more dissolved particles (higher i or higher m) means a bigger vapor-pressure suppression and a bigger elevation. The proportionality constant Kb is empirically measured for each solvent and folds in the solvent's molar mass and enthalpy of vaporization.
Inputs and what they mean
Molality (m) is used instead of molarity because it doesn't shift with temperature — the mass of solvent stays fixed even as the solution's volume changes slightly with heat. The van't Hoff factor (i) is the input most people get wrong: it's not the number of atoms in the solute, it's the number of independent particles it splits into in solution. Table sugar (sucrose) stays intact, so i=1; table salt splits into two ions, so i=2. Kb is solvent-specific — water's value of 0.512 °C·kg/mol is the one worth memorizing, since it appears in nearly every textbook problem.
Limits and edge cases
The ideal van't Hoff factor assumes complete dissociation, which holds well at low, dilute concentrations but breaks down as concentration rises — ions start re-pairing (ion pairing), so the effective i drops below the ideal integer value. For precise work at high concentrations, use an experimentally measured i rather than the theoretical value. The formula also assumes the solute is non-volatile (it doesn't itself evaporate and contribute vapor pressure) — for volatile solutes like alcohol in water, this simple model doesn't apply and Raoult's law for mixed volatiles is needed instead.