two solutions. Solvent molecules may pass through the membrane in either direction, but
the rate at which they pass into the more concentrated solution is found to be greater
than the rate in the opposite direction. The initial difference between the two rates is
directly proportional to the difference in concentration between the two solutions. Solvent
particles continue to pass through the membrane (Figure 14-16a). The column of liquid
continues to rise until the hydrostatic pressure due to the weight of the solution in the
column is sufficient to force solvent molecules back through the membrane at the same
rate at which they enter from the dilute side. The pressure exerted under this condition
is called the osmotic pressureof the solution.
Figure 14-16 (a) Laboratory
apparatus for demonstrating osmosis.
The picture at the right gives some
details of the process, which is
analogous to the transfer of solvent
into a solution through the space
above them (b). In (a) the solute
particles cannot pass through the
semipermeable membrane. In (b) the
solute particles cannot pass through
the vapor phase because they are
nonvolatile.
14-15 Osmotic Pressure 571
See the Saunders Interactive
General Chemistry CD-ROM,
Screen 14.9, Colligative Properties (3):
Osmosis.
Thistle tube
Level at start
Sugar solution
Rubber band
Membrane Water
Solution level
after osmosis
has progressed
for a time
Sugar
molecules
cannot pass
through
membrane
Some H 2 O
molecules
pass out of
the solution
Water molecules pass
in through membrane
(a)
(b)
Start Later
Start Later
Solution Solvent
Solution