The amount of solute that will dissolve in a given amount of solvent
Types of solutions
Unsaturated solution
Saturated solution
Supersaturated solution
Unsaturated solution
More solute dissolves
Saturated solution
No more solute dissolves
Supersaturated solution
Becomes unstable, crystals form
Principle of solubility
Like dissolves like - pertains to the similarity in the polarity of substances
Temperature
Solubility increases of most solids dissolved in water
Higher temperatures increase the vibration or kinetic energy of the solute molecules
Temperature increases
Solubility of gases decreases
Pressure
Only affects the solubility of gases - as pressure increases, solubility of gases increases, and as pressure decreases, solubility decreases
Colligative properties
Physical changes that result from adding solute to a solvent, depend only on the number of solute particles present, not on the identity of the solute particles
Colligative properties
Vapor pressure lowering
Freezing point depression
Boiling point elevation
Osmotic pressure
Vapor pressure lowering
The vapor pressure of a solution with a nonvolatile solute is always lower than that of the pure solvent
The relationship between the vapor pressure of the solution and the vapor pressure of the solvent depends on the concentration of the solute in the solution
Vapor pressure
The pressure exerted by the vapor particles on the liquid at equilibrium
Higher concentrations of non-volatile solutes make it harder for solvent to escape to the vapor phase, therefore the vapor pressure of a solution is lower than that of the pure solvent
Raoult's Law
The vapor pressure of a solution, PA, is equal to the mole fraction of the solvent, Xa times the vapor pressure of the pure solvent, PA
Boiling point elevation
The change in boiling point is proportional to the molality of the solution
Freezing point depression
The change in freezing point can be found similarly to boiling point elevation
Osmosis
A process through which a solvent flows through a semipermeable membrane from a less concentrated solution to a more concentrated one
Osmotic pressure
The amount of pressure required to stop the osmosis
Types of osmotic concentration
Hypotonic
Isotonic
Hypertonic
Hypotonic
The solute concentration is lower outside of the cell than that inside the cell, causing the cell to take in water and swell
Isotonic
The water outside of the cell has an EQUAL amount of salt as the water INSIDE of the cell, causing no change in cell size
Hypertonic
The solute concentration is higher outside than that inside the cell, causing it to shrivel and shrink
osmosis is also known as water diffusion
higher temperature increases the kinetic energy/vibration of solute molecule