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 core insight

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 x2x_2 this lowering is

p10−p1p10=x2=n2n1+n2≈n2n1 (dilute solution)\dfrac{p_1^0-p_1}{p_1^0} = x_2 = \dfrac{n_2}{n_1+n_2} \approx \dfrac{n_2}{n_1}\ (\text{dilute solution})

where p10p_1^0 is the pure solvent's vapour pressure, p1p_1 is the solution's vapour pressure, and n1n_1, n2n_2 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:

ΔTb=Kb m\Delta T_b = K_b\, m

where: ΔTb=Tb−Tb0\Delta T_b = T_b - T_b^0 is the rise in boiling point, mm is molality (mol of solute per kg of solvent), and KbK_b 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:

ΔTf=Kf m\Delta T_f = K_f\, m

where ΔTf=Tf0−Tf\Delta T_f = T_f^0 - T_f and KfK_f 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 Π\Pi 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:

Π=CRT\Pi = CRT

where CC is molar concentration (mol L⁻¹), RR is the gas constant, and TT 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.

Figure
Vapour pressure curves of pure solvent and solution showing the solution curve shifted below the solvent curve so it meets one atmosphere at a higher temperature and freezes at a lower temperature
Vapour pressure lowering shifts both boiling and freezing points temperature vapour pressure 1 atm pure solvent solution Tb0 Tb solution boils hotter and freezes colder than the pure solvent

Getting to molar mass. Every equation above hides n2=w2/M2n_2 = w_2/M_2, the moles of solute expressed as mass over molar mass. Once ΔTb\Delta T_b, ΔTf\Delta T_f, or Π\Pi is measured in the lab, the equation can be rearranged to solve for the one unknown, M2M_2.

Derivation AMolar mass from boiling point elevation

The goal is to turn a single measured temperature rise, ΔTb\Delta T_b, together with the known masses of solute and solvent used to make the solution, into the unknown molar mass M2M_2 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 ΔTb=Kb m\Delta T_b = K_b\, m, where KbK_b is a known constant of the solvent (looked up or given) and mm is the molality of the solution actually prepared. Rearranging for molality alone, m=ΔTb/Kbm = \Delta T_b / K_b.

Step 2. Expand molality using its own definition, moles of solute per kilogram of solvent: m=n2w1(kg)m = \dfrac{n_2}{w_1(\text{kg})}, where w1w_1 is the mass of solvent used. Since n2=w2/M2n_2 = w_2/M_2 (mass of solute over its molar mass), this becomes m=w2/M2w1(kg)m = \dfrac{w_2/M_2}{w_1(\text{kg})}.

Step 3. Set the two expressions for mm equal to each other: ΔTbKb=w2/M2w1(kg)\dfrac{\Delta T_b}{K_b} = \dfrac{w_2/M_2}{w_1(\text{kg})}. Every quantity here is known from the experiment except M2M_2, which is exactly what we are solving for.

Step 4. Cross-multiply and isolate M2M_2: M2=Kb w2ΔTb w1(kg)M_2 = \dfrac{K_b\, w_2}{\Delta T_b\, w_1(\text{kg})}. This is the working formula — plug in the solvent's KbK_b, the mass of solute w2w_2, the mass of solvent w1w_1 in kilograms, and the measured elevation ΔTb\Delta T_b, and M2M_2 falls out directly. The identical algebra, with KfK_f and ΔTf\Delta T_f in place of KbK_b and ΔTb\Delta T_b, 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 R=0.0821 L atm K−1mol−1R = 0.0821\ \text{L atm K}^{-1}\text{mol}^{-1}.)

Step 1. Write the van't Hoff equation and solve for concentration: Π=CRT  ⟹  C=ΠRT=4.920.0821×300\Pi = CRT \implies C = \dfrac{\Pi}{RT} = \dfrac{4.92}{0.0821 \times 300}.

Step 2. Compute the denominator and divide: C=4.9224.63=0.1998≈0.200 mol L−1C = \dfrac{4.92}{24.63} = 0.1998 \approx 0.200\ \text{mol L}^{-1}.

Step 3. Relate CC to molar mass using n2=w2/M2n_2 = w_2/M_2, with 6.0 g of solute in 1.0 L of solution: C=w2/M2V  ⟹  0.200=6.0/M21.0C = \dfrac{w_2/M_2}{V} \implies 0.200 = \dfrac{6.0/M_2}{1.0}.

Step 4. Solve for M2M_2: M2=6.00.200=30 g mol−1M_2 = \dfrac{6.0}{0.200} = 30\ \text{g mol}^{-1}.

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 ΔTb=Kbw2M2 w1(kg)=0.52×6.030×0.050=2.08 K\Delta T_b = \dfrac{K_b w_2}{M_2\, w_1(\text{kg})} = \dfrac{0.52 \times 6.0}{30 \times 0.050} = 2.08\ \text{K} — 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 ΔTb\Delta T_b, 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 ΔTb\Delta T_b, but Π=CRT\Pi = CRT still produces a comfortably measurable pressure.

Common traps

  • Mixing up molality and molarity. ΔTb\Delta T_b and ΔTf\Delta T_f use molality mm (moles of solute per kilogram of solvent); Π=CRT\Pi = CRT uses molarity CC (moles of solute per litre of solution) — using volume where mass is required, or vice versa, is the single most common slip.
  • Sign confusion. ΔTb=Tb−Tb0\Delta T_b = T_b - T_b^0 is a rise; ΔTf=Tf0−Tf\Delta T_f = T_f^0 - T_f 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 ΔTb=Kbm\Delta T_b = K_b m or Π=CRT\Pi = CRT underestimate the effect; that correction (the van't Hoff factor) belongs to the abnormal molar mass topic that follows this one.
  • Treating KbK_b or KfK_f 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 ΔTb\Delta T_b 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 RTRT multiplier in Π=CRT\Pi = CRT 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 ΔTf\Delta T_f comes out positive, matching the physical fact that the solution freezes at a lower temperature than the pure solvent (Tf0T_f^0 is the higher, pure-solvent value). Writing it the other way round, Tf−Tf0T_f - T_f^0, would make ΔTf\Delta T_f negative for every real solution, which is inconvenient to carry through the rest of the calculation. Boiling point elevation is written the opposite way, Tb−Tb0T_b - T_b^0, because there the solution's boiling point is the higher one, so that convention also keeps ΔTb\Delta T_b 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 n2=w2/M2n_2 = w_2/M_2, 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 ΔTb\Delta T_b or ΔTf\Delta T_f with everyday quantities of solute, so those are the standard laboratory routes. Very large molar masses need osmotic pressure instead, because ΔTb\Delta T_b and ΔTf\Delta T_f 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.

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