OUTLINE
The Dissolution Process
14-1 Spontaneity of the Dissolution
Process
14-2 Dissolution of Solids in Liquids
14-3 Dissolution of Liquids in
Liquids (Miscibility)
14-4 Dissolution of Gases in Liquids
14-5 Rates of Dissolution and
Saturation
14-6 Effect of Temperature on
Solubility
14-7 Effect of Pressure on Solubility
14-8 Molality and Mole Fraction
Colligative Properties of Solutions
14-9 Lowering of Vapor Pressure
and Raoult’s Law
14-10 Fractional Distillation
14-11 Boiling Point Elevation
14-12 Freezing Point Depression
14-13 Determination of Molecular
Weight by Freezing Point
Depression or Boiling Point
Elevation
14-14 Colligative Properties and
Dissociation of Electrolytes
14-15 Osmotic Pressure
Colloids
14-16 The Tyndall Effect
14-17 The Adsorption Phenomenon
14-18 Hydrophilic and Hydrophobic
Colloids
A
OBJECTIVES
After you have studied this chapter, you should be able to
- Describe the factors that favor the dissolution process
- Describe the dissolution of solids in liquids, liquids in liquids, and gases in liquids
- Describe how temperature and pressure affect solubility
- Express concentrations of solutions in terms of molality and mole fractions
- Describe the four colligative properties of solutions and some of their applications
- Carry out calculations involving the four colligative properties of solutions: lowering of
vapor pressure (Raoult’s Law), boiling point elevation, freezing point depression and
osmotic pressure - Use colligative properties to determine molecular weights of compounds
- Describe dissociation and ionization of compounds, and the associated effects on
colligative properties - Recognize and describe colloids: the Tyndall effect, the adsorption phenomenon,
hydrophilic and hydrophobic colloids
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solution is defined as a homogeneous mixtureof substances in which no settling occurs.
A solution consists of a solvent and one or more solutes, whose proportions vary from
one solution to another. By contrast, a pure substance has fixed composition. The
solventis the medium in which the solutesare dissolved. The fundamental units of solutes
are usually ions or molecules.
Spreading a soluble salt such as
calcium chloride on icy roadways or
sidewalks forms a solution with a
lower freezing point than pure
water, causing the ice or snow to
melt at a lower temperature.