Boiling Point/Freezing Point Calculator

Colligative Properties Calculator

Calculate boiling point elevation and freezing point depression.

ΔTₙ = i * Kₙ * m

The Effect of Solutes: A Guide to Colligative Properties

In chemistry, colligative properties are properties of solutions that depend on the ratio of the number of solute particles to the number of solvent molecules in a solution, and not on the nature of the chemical species present. In simpler terms, these properties depend on *how many* particles are dissolved, not *what* those particles are. Two of the most important colligative properties are boiling point elevation and freezing point depression.

When you dissolve a non-volatile solute (like salt or sugar) into a solvent (like water), the resulting solution will have a higher boiling point and a lower freezing point than the pure solvent. This is why we salt roads in the winter to prevent ice from forming and why the water in your car's radiator, which contains antifreeze, doesn't boil over in the summer. The extent of this change is directly proportional to the concentration of the solute particles. This calculator is a tool that allows you to quantify these effects, making it essential for students learning about solution chemistry and for anyone working in a lab where the physical properties of solutions are important.

The Formulas for Boiling Point Elevation and Freezing Point Depression

Both phenomena are described by very similar formulas:

  • Boiling Point Elevation: ΔTₙ = i * Kₙ * m
  • Freezing Point Depression: ΔT₟ = i * K₟ * m

Where:

  • ΔT is the change in temperature (°C). For boiling, this is the amount the boiling point increases. For freezing, it's the amount the freezing point decreases.
  • i is the van 't Hoff factor. This is the number of individual particles (ions) the solute dissociates into when dissolved. For non-electrolytes like sugar, i=1. For electrolytes like NaCl (which splits into Na⁺ and Cl⁻), i=2. For CaCl₂, i=3.
  • K is the molal constant of the solvent. Kₙ is the ebullioscopic constant (for boiling), and K₟ is the cryoscopic constant (for freezing). These are unique for each solvent. For water, Kₙ ≈ 0.512 °C·kg/mol and K₟ ≈ 1.86 °C·kg/mol.
  • m is the molality of the solution, which is the moles of solute per kilogram of solvent (mol/kg).

Why Do These Effects Happen?

Both boiling point elevation and freezing point depression are results of the solute particles interfering with the phase transition process of the solvent molecules.

  • Boiling Point Elevation: For a liquid to boil, its vapor pressure must equal the surrounding atmospheric pressure. Solute particles effectively "get in the way" of solvent molecules at the surface, reducing the number of solvent molecules that can escape into the vapor phase. This lowers the solution's vapor pressure. To overcome this and make the solution boil, you need to add more energy in the form of heat, which results in a higher boiling point.
  • Freezing Point Depression: For a liquid to freeze, its molecules must arrange themselves into a highly ordered crystal lattice. Solute particles disrupt this process, getting in the way and making it more difficult for the solvent molecules to form a solid structure. To make the solution freeze, you have to remove more energy from it (i.e., make it colder) than you would for the pure solvent. This results in a lower freezing point.

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