Osmosis is the movement of water through a plasma membrane from a region of low solute concentration to a region of high concentration. It is a type of diffusion. Osmosis is passive transport, meaning it does not require energy to be applied. What causes osmotic pressure is different concentrations of solutes on the two sides of the membrane.
When osmosis happens, water moves from the side of the membrane with a lower amount of osmotic pressure to the side of the membrane with the higher amount. An important example of osmosis is the movement of liquid (solvent) molecules across a cell membrane into a cell with a higher solute concentration. Osmosis is a fundamental part of cell biochemistry, but also has mechanical applications and usages.
Hypotonic, isotonic, and hypertonic[change | change source]
Hypotonic describes the less concentrated solution. An isotonic solution is when the concentration is equal on both sides of the membrane. Hypertonic describes the more concentrated solution. The usual cell distortion situation is: hypotonic solution outside the cell, and hypertonic solution inside.
Cell membranes[change | change source]
The plasma membrane of a cell is semi-permeable, which means it lets small molecules pass through, but blocks larger molecules. The membrane also has ports or gateways which get certain macromolecules through. This is active transport, which uses energy and is selective.
References[change | change source]
- http://physioweb.med.uvm.edu/bodyfluids/osmosis.htm University of Vermont, Department of Physiology