Ensure labs are submitted ASAP to avoid losing credit.
Grading of routines is coming soon.
Focus on freezing point and boiling point.
Exam will include:
Freezing Point
Boiling Point
Osmotic Pressure
Vapor Pressure
Note: Conductivity is not a colligative property.
Colligative properties are defined as properties that change as solute is added to a solvent.
As solute amount increases, changes in boiling and freezing points increase proportionately.
Change in properties is gradual with solute addition.
Sample values discussed:
Freezing Point:
Q1: -14°C
Q2: -18.6°C
Q3: -32°C
Q4: -15°C
Boiling Points:
Q1: 103.9°C
Q2: 105.2°C
Q3: 108.8°C
Q4: 104.2°C
Notable Points:
Ions affect calculations for freezing and boiling points (i-value).
Example values and points emphasized for clarity.
Osmotic Pressure (π) relates to concentration and is influenced by the number of particles (ions) from solute.
Important concepts:
Osmosis involves water moving from areas of high concentration to areas of low concentration.
Osmotic pressure is the pressure exerted by the water molecules when they pass through a semi-permeable membrane.
Key Equation:
π = i x M x R x T
where:
π = osmotic pressure
i = ionization factor
M = molarity
R = gas law constant
T = temperature in Kelvin
Molarity includes units of moles and liters, clarifying the relationship with pressure volume equations.
Relation to PV = nRT discussed, showing how to rearrange for concentration.
Ionization factors (i-values) discussed using common examples:
Sucrose (not ionizing, i=1)
Sodium Chloride (NaCl, dissociates i=2)
Calcium Chloride (CaCl2, dissociates i=3)
Example problems were worked through to reinforce learning.
Experiment with dialysis tubing highlighted:
Used to demonstrate osmotic pressure and the movement of water through semi-permeable membranes.
Defined terms:
Hypertonic: higher solute concentration, draws water out.
Hypotonic: lower solute concentration, draws water in.
Isotonic: equal concentrations of solute.
Observations of mass changes based on water movement proved key in evaluating osmotic pressure.
Explanation of how solutes affect solubility and osmotic pressure when present together (common ions).
Example using sodium chloride and potassium chloride, demonstrating how to calculate concentrations of common ions:
Use of mole ratios to figure out the concentration of individual ions in solutions.
Practical calculations demonstrated including total ion concentrations using examples from previous lessons.
Assigned homework on osmosis, reinforcing the diffusion of water and osmotic pressure calculations.
Encouraged students to visualize their steps and present data appropriately in lab settings.