Reverse Osmosis (RO) Water


Reverse osmosis (RO) is a membrane-technology filtration method that removes many types of large molecules and ions from solutions by

applying pressure to the solution when it is on one side of a selective membrane. The result is that the solute is retained on the

pressurized side of the membrane and the pure solvent is allowed to pass to the other side. To be "selective," this membrane should

not allow large molecules or ions through the pores (holes), but should allow smaller components of the solution (such as the

solvent) to pass freely.


In the normal osmosis process, the solvent naturally moves from an area of low solute concentration (High Water Potential), through a

membrane, to an area of high solute concentration (Low Water Potential). The movement of a pure solvent to equalize solute

concentrations on each side of a membrane generates osmotic pressure. Applying an external pressure to reverse the natural flow of

pure solvent, thus, is reverse osmosis. The process is similar to other membrane technology applications. However, there are key

differences between reverse osmosis and filtration. The predominant removal mechanism in membrane filtration is straining, or size

exclusion, so the process can theoretically achieve perfect exclusion of particles regardless of operational parameters such as

influent pressure and concentration. Moreover, reverse osmosis involves a diffusive mechanism so that separation efficiency is

dependent on solute concentration, pressure, and water flux rate.[1] Reverse osmosis is most commonly known for its use in drinking

water purification from seawater, removing the salt and other effluent materials from the water molecules.