“…Colligative properties of solutions, such as osmotic pressure, boiling point elevation, and freezing point depression, are properties that only depend on the number of dissolved solutes but not their identity. Common, longstanding chemistry laboratory curriculum experiments involve the determination of the molecular weight of nondissociable organic solutes by means of the boiling point elevation or freezing point depression, − recognizing that absolute change in phase transition temperature relative to the pure solvent, Δ T , is proportional to the solute molality, m , according to eq with K being either the molal freezing point depression or boiling point elevation constant. An underlying assumption in eq is that the solute does not aggregate, which is the case for many organic solutes in organic solvents. Conversely, solute aggregation is in principle detectable by a lesser Δ T than expected from solution molality.…”