When the following solutions are brought into touch with one another on various sides of a semipermeable membrane, the net direction that water would diffuse (via osmosis) is that Water travels through osmosis from low solute concentration areas to high solute concentration areas.
Osmosis is the naturally occurring diffusion or passage of water or other solvents over a semipermeable membrane (one that prevents the passage of solutes, or dissolved compounds).
German plant physiologist Wilhelm Pfeffer began a systematic study of the crucial biological process in 1877.
Both the pressure gradient and the concentration gradient affect the net direction and rate of osmosis.
Hypertonic, isotonic, and hypotonic are the three osmotic states.
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