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Untitled - Kelly Walsh High School

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Solutions 179<br />

Just as the freezing point of a solution is always lower than the pure solvent, the<br />

boiling point of a solution is always higher than the solvent. The relationship is<br />

similar to the one for the freezing point depression above and is:<br />

T b iK bm<br />

In this equation, T b is the number of degrees that the boiling point has been<br />

elevated (the difference between the boiling point of the pure solvent and the<br />

solution), K b is the boiling-point elevation constant, m is the molality of the<br />

solute, and i is again the van’t Hoff factor.<br />

Osmotic Pressure<br />

A U-tube contains a solution and pure solvent. A semipermeable membrane separates<br />

the two components. Such a membrane allows the passage of solvent molecules<br />

but not solute particles. This arrangement will result in the level of the solvent<br />

side decreasing while the solution side increasing. This indicates that the solvent<br />

molecules are passing through the semipermeable membrane. This process is<br />

osmosis. Eventually the system would reach equilibrium and the difference in levels<br />

would remain constant. The difference in the two levels is related to the osmotic<br />

pressure. In fact, one could exert a pressure on the solution side exceeding the<br />

osmotic pressure. This will cause the solvent molecules to move back through the<br />

semipermeable membrane into the solvent side. This process is reverse osmosis<br />

and is the basis of desalination of seawater for drinking purposes.<br />

The osmotic pressure is a colligative property and mathematically represented as:<br />

(nRT/V) i iMRT<br />

In this equation, is the osmotic pressure in atmospheres, n is the number of<br />

moles of solute, R is the ideal gas constant (0.0821 L . atm/Kmol), T is the<br />

Kelvin temperature, V is the volume of the solution and i is the van’t Hoff factor.<br />

If one knows the moles of solute and the volume in liters, n/V may be<br />

replaced by the molarity, M. It is possible to calculate the molar mass of a solute<br />

from osmotic pressure measurements. This is especially useful in the determination<br />

of the molar mass of large molecules such as proteins.<br />

12-4 Colloids<br />

Particles will settle out of water from a muddy stream. This water is a heterogeneous<br />

mixture, where the particles are large (in excess of 10 3 nm in diameter)<br />

and is a suspension. On the other hand, dissolving sodium chloride in water produces<br />

a true homogeneous solution, where the solute particles are less than<br />

1 nm in diameter. Particles do not settle out of a true solution because of their<br />

very small particle size. However, there is a mixture with particle diameters

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