As soon as the water passes through the diaphragm, the pressure decreases on the less concentrated side. Simultaneously, the pressure of the more concentrated solution increases until a balance is reached, which stops the flow through the diaphragm.
The difference in pressure between the two solutions in such a balanced state is called “osmotic pressure”.
Reverse osmosis is a scientific reversion procedure of the natural osmotic process: all that is needed is the application of a greater pressure than the osmotic pressure to reverse the flow in the semi-permeable diaphragm and therefore to separate the salts and the dissolved solids.
Before this process was possible, a synthetic diaphragm had to be designed, which needed to be highly permeable to water but which also needed to act as an effective barrier against salts and all the other dissolved minerals. |