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Chemistry class 12th Osmosis and osmotic pressure

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Osmosis is the movement of water molecules through a semipermeable membrane from a region of lower solute concentration to higher concentration, aiming to equalize concentrations on both sides. This natural process is essential in biological systems, such as nutrient absorption in cells. Osmotic pressure is the pressure required to stop this water movement. It depends on solute concentration—the higher the concentration, the greater the osmotic pressure. This principle is used in medical treatments (e.g., IV fluids) and industrial applications like water purification. Reverse osmosis, a related process, applies external pressure to force water against its natural osmotic gradient.

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Osmosis and Osmotic Pressure


1. Introduction

Osmosis is the process of movement of solvent molecules from a region of lower solute
concentration to a region of higher solute concentration through a semipermeable membrane. This
process continues until equilibrium is reached.


Osmotic pressure is the pressure required to stop the osmosis process. It is a colligative property
that depends on the concentration of solute particles, not their identity.


2. Definition and Explanation


**Osmosis:** The spontaneous movement of solvent molecules across a semipermeable membrane
toward a higher solute concentration.


**Osmotic Pressure:** The minimum pressure needed to prevent the net movement of solvent
molecules through a semipermeable membrane.


3. Formula and Derivation


Osmotic pressure (Pi) is given by Van't Hoff's equation:


Pi = nRT / V


or in terms of molarity (C):
Pi = CRT


where:
- Pi = Osmotic pressure
- C = Molar concentration of the solution (mol/L)
- R = Universal gas constant (0.0821 L atm mol-¹ K-¹)
- T = Temperature in Kelvin
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