Title: Colligative properties of solutions
1Colligative properties of solutions
- The Effects of Solutes on Solvents
2Objectives
- When you complete this presentation, you will be
able to - define a colligative property
- explain how colligative properties are dependent
on the number of particles in solution - describe the effects on the numbers of particles
in a solution on the vapor pressures, freezing
points, boiling points, and osmotic pressures of
those solutions
3Introduction
- The physical properties of a solution differ from
the properties of the pure solvent. - Salt added to water decreases the freezing point
of the solution. - Copper(II) sulfate added to water changes the
color. - When a property depends on the number of
particles of solute in a solution, that is a
colligative property.
4Introduction
- Colligative properties depend only on the number
of solute particles, not on identity of the
solute. - Different solutes produce different numbers of
solute particles when they are dissolved. - Ionic compounds produce more particles per mol of
solute dissolved than do molecular compounds.
5Introduction
- For example
- NaCl produces two mols of particles for each mol
of salt dissolved - 1 mol of Na
- and
- 1 mol of Cl-
- Glucose, C6H12O6, produces one mol of particles
for each mol of glucose dissolved.
6Introduction
- There are many different kinds of colligative
properties. - Important colligative properties of solutions
that we will study include - vapor-pressure lowering
- freezing-point depression
- boiling-point elevation
- osmotic pressure increase
7Vapor-pressure lowering
- Vapor pressure is the pressure exerted by a vapor
that is in equilibrium with its liquid in a
closed system. - When we add a solute to pure liquid, we reduce
the number of particles of liquid that are
available to be converted to vapor.
8Vapor-pressure lowering
- In the pure liquid, there are 8 solvent particles
available to go into vapor. - In the solution, there are only 6 solvent
particles available to go into vapor.
9Vapor-pressure lowering
- If we have more solute, there are even fewer
solvent particles available.
10Vapor-pressure lowering
- If we have fewer solute, there are more solvent
particles available.
11Vapor-pressure lowering
- The decrease in vapor pressure is proportional to
the number of particles in solution. - Adding one mol of NaCl produces twice the vapor
pressure lowering of adding one mol of glucose.
12Freezing-point depression
- Adding a solute to a solvent lowers the freezing
point of the solution. - The lowering is proportional to the number of
particles of the solute added to the solvent. - 1 mole of glucose added to 1 kg of water results
in a fp lowering of 1.86C. - 1 mole of NaCl added to 1 kg of water results in
a fp lowering of 3.72C.
13Freezing-point depression
- This is used for -
- keeping the roads ice-free in the winter
- adding antifreeze to your car
14Boiling-Point elevation
- Adding a solute to a solvent also raises the
boiling point of the solution. - The elevation is also proportional to the number
of particles of the solute added to the solvent. - 1 mole of glucose added to 1 kg of water results
in a bp elevation of 0.51C. - 1 mole of NaCl added to 1 kg of water results in
a bp elevation of 1.02C.
15Boiling-Point elevation
- This is used for -
- adding to your cars cooling system for the summer
16Osmotic Pressure
- Osmosis is the spontaneous movement of solvent
molecules through a partially permeable membrane
into an area of higher solute concentration. - This process is used extensively in biological
systems. - Biological membranes are semipermeable.
17Osmotic Pressure
In an osmotic cell, we have two solutions of
different concentrations divided be a
semipermeable membrane.
18Osmotic Pressure
Pure water will move through the semipermeable
membrane from the cell on the right into the cell
on the left.
19Osmotic Pressure
This causes the water level on the left to rise
and the water level on the right to fall.
20Osmotic Pressure
This causes the water level on the left to rise
and the water level on the right to fall.
21Osmotic Pressure
At a certain point, the pressure from the height
of the water on the left will cause water to flow
back into the cell on the right and the system
will come to an equilibrium.
22Osmotic Pressure
The difference in liquid levels between the two
cells is a measure of the osmotic pressure of the
system.
23Osmotic Pressure
A system with a greater number of solute
particles in one cell will have a greater osmotic
pressure.
24Osmotic Pressure
A system with a greater number of solute
particles in one cell will have a greater osmotic
pressure.
25Osmotic Pressure
If we raise the solution level of the left cell
only, there will be more pressure to move pure
water to the right than there is pressure to move
water to the left.
26Osmotic Pressure
If we raise the solution level of the left cell
only, there will be more pressure to move pure
water to the right than pressure to move water to
the left.
27Osmotic Pressure
Water will move from the left cell to the right
cell until the equilibrium is reestablished.
28Osmotic Pressure
This is called reverse osmosis and is used around
the world to purify water.
29Osmotic Pressure
Membranes are fragile and expensive, so the
process is used only where other purification
systems will not work.
30Summary
- The physical properties of a solution differ from
the properties of the pure solvent. - When a property depends on the number of
particles of solute in a solution, that is a
colligative property. - Colligative properties depend only on the number
of solute particles, not on identity of the
solute. - Ionic compounds produce more particles per mol of
solute dissolved than do molecular compounds.
31Summary
- Important colligative properties of solutions
include vapor-pressure lowering, freezing-point
depression, and boiling-point elevation. - When we add a solute to pure liquid we -
- reduce the vapor pressure that is exerted over
the surface of the liquid. - lower the freezing point of the liquid.
- raise the boiling point of the liquid.
- increase the osmotic pressure of the liquid.