Colligative Properties and Molar Mass
Dissolve one gram of an unknown white powder in fifty grams of water and something measurable happens: the solution boils a little above 100 degrees Celsius, freezes a little below zero, and can hold back an invading flow of pure water across a membrane. None of these effects care whether the powder is sugar, urea, or some unnamed compound — they depend only on how many solute particles are floating in the solvent. Properties with this "just count the particles" character are called colligative properties, and there are exactly four of them: relative lowering of vapour pressure, boiling point elevation, freezing point depression, and osmotic pressure. Because each one is governed by a simple, measurable equation containing the solute's molar mass as the only unknown, colligative properties turn an ordinary boiling-point or osmotic-pressure measurement into a working balance for weighing molecules too small to put on a scale.
The four colligative properties — vapour pressure lowering, boiling point elevation, freezing point depression, and osmotic pressure — depend only on the number of solute particles, so measuring any one of them and rearranging its formula gives the solute's molar mass.
The core idea
Why "colligative." A dilute solution of a non-volatile, non-electrolyte solute (one mole of solute gives exactly one mole of dissolved particles, and the solute does not evaporate) shows four linked effects, all traceable to the same cause: dissolved solute particles get in the way of solvent molecules escaping into vapour, so the solution's vapour pressure is lower than the pure solvent's at every temperature.
1. Relative lowering of vapour pressure. For a solute mole fraction this lowering is
where is the pure solvent's vapour pressure, is the solution's vapour pressure, and , are moles of solvent and solute.
2. Boiling point elevation. Because the solution's vapour pressure curve sits below the pure solvent's, it takes a higher temperature to push the vapour pressure back up to 1 atmosphere, so the solution boils hotter:
where: is the rise in boiling point, is molality (mol of solute per kg of solvent), and is the molal elevation constant of the solvent (units K kg mol⁻¹) — a fixed property of the solvent, never of the solute.
3. Freezing point depression. The same vapour-pressure argument, run at the freezing point instead, gives a lower freezing point for the solution:
where and is the molal depression constant (cryoscopic constant) of the solvent.
4. Osmotic pressure. Osmosis is the spontaneous flow of solvent through a semipermeable membrane toward the more concentrated side; osmotic pressure is the extra pressure needed on the solution side to stop that net flow. For dilute solutions it obeys a van't Hoff equation shaped exactly like the ideal gas law:
where is molar concentration (mol L⁻¹), is the gas constant, and is absolute temperature. The figure below shows why boiling point rises and freezing point falls together: the solution's vapour-pressure curve is uniformly shifted down, so it crosses the 1-atm line at a higher temperature and crosses the solid-liquid line at a lower one.
Getting to molar mass. Every equation above hides , the moles of solute expressed as mass over molar mass. Once , , or is measured in the lab, the equation can be rearranged to solve for the one unknown, .
The goal is to turn a single measured temperature rise, , together with the known masses of solute and solvent used to make the solution, into the unknown molar mass of the solute, using nothing beyond the definition of molality and simple algebra — no calculus is needed anywhere in this derivation.
Step 1. Start from the defining relation , where is a known constant of the solvent (looked up or given) and is the molality of the solution actually prepared. Rearranging for molality alone, .
Step 2. Expand molality using its own definition, moles of solute per kilogram of solvent: , where is the mass of solvent used. Since (mass of solute over its molar mass), this becomes .
Step 3. Set the two expressions for equal to each other: . Every quantity here is known from the experiment except , which is exactly what we are solving for.
Step 4. Cross-multiply and isolate : . This is the working formula — plug in the solvent's , the mass of solute , the mass of solvent in kilograms, and the measured elevation , and falls out directly. The identical algebra, with and in place of and , gives molar mass from freezing point depression instead.
Worked example
Problem: A solution containing 6.0 g of a non-volatile, non-electrolyte solute dissolved in 1.0 L of solution has an osmotic pressure of 4.92 atm at 300 K. Calculate the molar mass of the solute. (Use .)
Step 1. Write the van't Hoff equation and solve for concentration: .
Step 2. Compute the denominator and divide: .
Step 3. Relate to molar mass using , with 6.0 g of solute in 1.0 L of solution: .
Step 4. Solve for : .
The solute has a molar mass of 30 g mol⁻¹.
Competitive stretch
The same 6.0 g sample, if instead dissolved in 50 g of water, would raise the boiling point by — a rise nearly twenty times larger than the 0.104 K seen for the 1.0 g, 100 g mol⁻¹ solute of the earlier boiling-point example. This is exactly why osmotic pressure, not , is preferred for very large solute molar masses such as proteins and polymers: their tiny molar concentration at reasonable working masses gives an almost unmeasurable , but still produces a comfortably measurable pressure.
Common traps
- Mixing up molality and molarity. and use molality (moles of solute per kilogram of solvent); uses molarity (moles of solute per litre of solution) — using volume where mass is required, or vice versa, is the single most common slip.
- Sign confusion. is a rise; is written the opposite way round so that it too comes out positive — plugging temperatures in mechanically without checking the direction flips the sign of the answer.
- Applying these formulas unmodified to electrolytes. NaCl, CaCl₂, and other electrolytes dissociate into more particles than moles dissolved, so plain or underestimate the effect; that correction (the van't Hoff factor) belongs to the abnormal molar mass topic that follows this one.
- Treating or as solute properties. Both constants belong to the solvent alone and never change with which solute is dissolved in it.
Ask the tutor: not sure which colligative-property formula to reach for given a problem's units, or want to practice more molar-mass calculations from freezing point or vapour pressure data — ask the AI tutor to walk through more examples.
Why does osmotic pressure work so much better than boiling point elevation for finding the molar mass of a protein?
A protein has an enormous molar mass, often tens of thousands of g/mol, so even several grams of it dissolved in water gives a tiny number of moles and therefore a tiny molality — the resulting can be a few thousandths of a degree, far too small to measure precisely with an ordinary thermometer. Osmotic pressure scales the same way with moles, but the multiplier in is large enough that even this tiny concentration produces an osmotic pressure of a fraction of an atmosphere, which is easily measured with standard apparatus. That is why osmotic pressure is the method of choice for macromolecules like proteins and polymers.
Why is the freezing point depression formula written as Tf zero minus Tf instead of Tf minus Tf zero?
It is purely a sign convention chosen so that comes out positive, matching the physical fact that the solution freezes at a lower temperature than the pure solvent ( is the higher, pure-solvent value). Writing it the other way round, , would make negative for every real solution, which is inconvenient to carry through the rest of the calculation. Boiling point elevation is written the opposite way, , because there the solution's boiling point is the higher one, so that convention also keeps positive.
Can I use any one of the four colligative properties to find the molar mass of any solute?
In principle yes, since all four contain , but in practice the choice depends on how large the effect is for the amount of solute you can conveniently dissolve. Small, ordinary molar masses (tens to a few hundred g/mol) give an easily measured or with everyday quantities of solute, so those are the standard laboratory routes. Very large molar masses need osmotic pressure instead, because and would be too small to read accurately. Relative lowering of vapour pressure is used less often experimentally because it is harder to measure precisely, even though the formula is equally valid.