Again, consider that ln xsolvent,solutionln(1 xsolute) xsolute. Making one
final substitution:
xsoluteRTV
This is usually rearranged to read as
VxsoluteRT (7.56)
This equation, which is a remarkable parallel to the ideal gas law, is called the
van’t Hoff equation,after Jacobus van’t Hoff, a Dutch physical chemist who an-
nounced this equation in 1886.* (He was also one of the originators of the con-
cept of the tetrahedral carbon atom, and was the first recipient of the Nobel
Prize for Chemistry in 1901.) The equation relates the osmotic pressure of a
solution to the mole fraction of the solute in the solution. It is strictly valid
only for very dilute solutions (reminiscent of many ideal gas systems), but is
also a useful guide for more concentrated ones.
Example 7.15
What is the osmotic pressure of a 0.010-molal solution of sucrose in water?
If this solution were placed in a system as illustrated in Figure 7.28, how
high would the column of diluted sucrose be at equilibrium if the tube has
a surface area of 100.0 cm^2? Assume 25°C, and that the density of the so-
lution is 1.01 g/mL. Some necessary conversions are 1 bar 105 pascal, and
1 pascal 1 N/m^2 (newton of force per square meter of area), and re-
member that Fmafor converting a mass into its equivalent force. (In this
case,awill be the acceleration due to gravity, which is 9.81 m/s^2 .)
Solution
A 0.010-molal solution contains 0.010 mole of sucrose in 1.00 kg, or 1000 g,
of water. In 1.00 kg of H 2 O, there are 1000 g/(18.01 g/mol) 55.5 mol H 2 O.
Therefore, the mole fraction of sucrose is
55.5
0
.01
0
0
.010
0.000180 xsolute
The molar volume of water is 18.01 mL, or 0.01801 L. Using the van’t Hoff
equation:
(0.01801 L)0.0001800.08314
m
L
o
b
l
a
K
r
298 K
0.248 bar
This is a substantial osmotic pressure for such a dilute solution! In order to
know how high the column will be, we convert this into N/m^2 :
0.248 bar
105
1
p
b
a
a
s
r
cals
1
1
p
N
a
/
s
m
ca
2
l
2.48 104 N/m^2
For a surface area of 100.0 cm^2 1.00 10 ^2 m^2 , this pressure is caused by
a force determined as
2.48 104
m
N
2 1.00 10
(^2) m (^2) 248 N
198 CHAPTER 7 Equilibria in Multiple-Component Systems
*This is different from the van’t Hoff equation introduced in Chapter 5.