Osmotic Pressure Simulation

Interactive demonstration of osmotic pressure, van't Hoff equation, solvent flow, and reverse osmosis

U-Tube Osmosis Experiment

Osmotic Pressure (Π): 0.00 atm
Height Difference: 0.00 cm
Applied Pressure: 0.00 atm
Flow Direction: None

Π vs Concentration

Current Point
Theoretical (Π = iMRT)

Parameters

Physical Equations

van't Hoff Equation: Π = iMRT
Ideal Gas Form: ΠV = nRT
Height Relation: Π = ρgh

Display Options

Solute Presets

Osmosis Mode

What is Osmotic Pressure?

Osmotic pressure is the minimum pressure needed to prevent the inward flow of a pure solvent across a semipermeable membrane. The semipermeable membrane allows solvent molecules to pass through but blocks solute particles. When two solutions of different concentrations are separated by such a membrane, solvent flows from the region of lower solute concentration (higher solvent concentration) to the region of higher solute concentration (lower solvent concentration). This natural flow creates a pressure difference that can be measured as osmotic pressure.

van't Hoff Equation

The van't Hoff equation, Π = iMRT, relates osmotic pressure (Π) to molarity (M), temperature (T), and the van't Hoff factor (i). The van't Hoff factor accounts for the number of particles a solute dissociates into in solution. For non-electrolytes like glucose, i = 1; for strong electrolytes like NaCl, i = 2 (one Na⁺ and one Cl⁻); for CaCl₂, i = 3 (one Ca²⁺ and two Cl⁻). The equation resembles the ideal gas law (PV = nRT), showing that osmotic pressure depends only on the number of solute particles, not their identity.

U-Tube Experiment

In a classic U-tube osmosis experiment, a semipermeable membrane separates two compartments. One contains pure solvent, the other a solution. Initially, both liquid levels are equal. As osmosis proceeds, solvent flows into the solution side, raising its level. The flow continues until the hydrostatic pressure from the height difference balances the osmotic pressure. At equilibrium, the height difference (h) relates to osmotic pressure by Π = ρgh, where ρ is the solution density and g is gravitational acceleration.

Reverse Osmosis

Reverse osmosis occurs when an external pressure greater than the osmotic pressure is applied to the solution side. This forces solvent to flow backward through the membrane from the solution to the pure solvent side. Reverse osmosis is widely used for water purification, desalination, and concentrating solutions. The minimum pressure required for reverse osmosis equals the osmotic pressure, but in practice, higher pressures are used to achieve reasonable flow rates. The process effectively separates solute from solvent, producing pure solvent from the solution side.

Applications

Osmotic pressure principles are essential in biology (maintaining cell turgor pressure, kidney function, and red blood cell behavior in different solutions), medicine (intravenous fluids must be isotonic with blood), food preservation (adding salt or sugar increases osmotic pressure, inhibiting microbial growth), water treatment (reverse osmosis desalination plants produce fresh water from seawater), and chemical industry (determining molecular weights of polymers and proteins through osmotic pressure measurements).