Boiling-Point Elevation
Also known as colligative boiling
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A non-volatile solute lowers the solvent's vapor pressure, so the solution must be heated a little hotter before that pressure reaches the atmosphere's — the boiling point rises. The rise depends only on how many particles are dissolved, not what they are, scaled by the solvent's ebullioscopic constant Kb. Water's Kb is a modest 0.512 K·kg/mol: a hearty 1.0 mol/kg sugar solution boils at just 100.5 °C, which is why salting pasta water changes its flavor far more than its physics.
Other solvents respond much more strongly — benzene's Kb is 2.53 and camphor's freezing-side cousin is famously huge — and remember that ionic solutes count each ion: 1 mol/kg NaCl acts as nearly 2 mol/kg of particles. Solved backwards, a measured ΔTb divided by Kb gives the molality, the classical route to a dissolved compound's molar mass before mass spectrometers existed.
- = Boiling-point elevation
- = Ebullioscopic constant
- = Molality of solution
- Boiling-point elevation — Freezing-Point Depression, Sensible Heat (Q = mcΔT)
- Ebullioscopic constant — Freezing-Point Depression
- Molality of solution — Freezing-Point Depression, Molality (b = n/m)