Osmosis Theory

Osmosis is the process where water molecules move across a semi-permeable membrane from an area with a lower concentration of solutes (like salt or sugar) to an area with a higher solute concentration. This movement aims to balance the concentrations on both sides of the membrane. The process is driven by the natural tendency of water to equalize solute differences, resulting in an increase in water volume on the side with more solutes. Osmosis is fundamental in many biological functions, such as water absorption in plant roots and fluid regulation in cells.