Osmosis is the flow of solvent from an area of higher solvent concentration to lower concentration. The equilibrium hydrostatic pressure resulting from osmosis is called osmotic pressure. There are three laws that govern osmotic pressure that are analogous to gas laws: 1) Boyle's law - osmotic pressure is proportional to concentration at constant temperature, 2) Charles' law - osmotic pressure is proportional to absolute temperature at constant concentration, 3) Avogadro's law - osmotic pressure is proportional to amount of solute. These laws allow derivation of an equation for osmotic pressure that is identical to the ideal gas law, indicating dilute solutions behave similarly to ideal gases.