Q.Isotonic solutions have the same:
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Osmotic Pressure: The Push of Pure Solvent
Imagine you have a U-shaped tube with a special membrane at the bottom that only lets water molecules pass through — not sugar molecules. On one side you put pure water, on the other side you put a sugar solution. What happens?
Water moves from the pure side into the solution side. The solution level rises. This is osmosis — the spontaneous net movement of solvent across a semipermeable membrane from a region of lower solute concentration to higher solute concentration.
But here's the key question: what if you don't want that level to rise? What if you want to keep the solution side exactly where it is?
You would have to push down on the solution side with extra pressure — just enough to stop the water from coming in. That extra pressure is osmotic pressure.
Osmotic pressure is not a pressure the solution "has" inside it. It is the external pressure you must apply to prevent osmosis. Think of it as the "resistance pressure" that exactly balances the tendency of solvent to dilute the solution.
The Precise Definition
Osmotic pressure () is the minimum excess pressure that must be applied to a solution to prevent the inward flow of solvent across a semipermeable membrane.
The membrane must be permeable only to solvent molecules, not to solute particles. This is the defining condition — if the membrane leaks solute, you don't get true osmotic pressure.
The van't Hoff Equation
For dilute solutions, osmotic pressure follows a beautifully simple law:
Where:
- = osmotic pressure (in atm or Pa)
- = molar concentration of solute (mol/L or mol/m³)
- = universal gas constant
- = absolute temperature (K)
This is van't Hoff's law of osmotic pressure. It looks exactly like the ideal gas law ( rearranged as ), and that's no coincidence — van't Hoff noticed that solute particles in dilute solution behave like gas molecules bouncing around, creating a "pressure" against the membrane.
This equation works only for non-electrolyte solutions at low concentrations. For electrolytes, you must include the van't Hoff factor : . A 0.1 M NaCl solution gives nearly twice the osmotic pressure of a 0.1 M glucose solution because NaCl dissociates into two ions.
Why It Matters for Macromolecules
Here's where osmotic pressure becomes a powerful tool. Suppose you have a protein — say, hemoglobin — and you want to know its molar mass. You can't easily measure its concentration in mol/L because you don't know the molar mass yet. But you can measure:
- The mass of protein dissolved (say, grams in liters)
- The osmotic pressure of that solution
Since , where is the molar mass:
Rearrange:
| Property | Why osmotic pressure wins |
|----------|---------------------------|
| Boiling point elevation | Very small for macromolecules — hard to measure |
| Freezing point depression | Very small — same problem | …
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