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Unsaturated solution
Has less than the maximum amount of solute dissolved in a solvent.
Saturated solution
Has the maximum amount of solute dissolved in a solvent. Adding more solute leads to it remaining undissolved.
Supersaturated
Happens when heated, the solution contains more dissolved solute than they can normally hold at a given temperature and pressure.
Crystallization
This occurs when a dissolved solute comes out of the solution. These crystals are generally formed by manipulating temperature or pressure.
What are the soluble salts?
Group 1 metal cations, NO3- CLO4- C2H3O2- and NH4- Note soluble component trumps the insoluble component.
What are the insoluble salts?
Ag+ Pb2+ Hg2+ OH- S2- CO32- PO43-
Electrolytes
Substances that have a natural positive or negative electrical charge when dissolved in water.
Strong Electrolytes
Fully dissociate in water
Soluble ionic compounds
Strong acids
Strong Bases
Weak electrolytes
Incompletely dissociate in water
Weak acids
Weak bases
Non-electrolyes
Do not dissociate in water
Molecular compounds that are not acidic or basic eg. C6H12O6, CH3OH, etc.
Strong Acids
HCl, HBr, HI, HClO4, HClO3, H2SO4, HNO3.
Strong Bases
Group I Metal Hydroxides (metal + OH), Ca(OH)2, Sr(OH)2, Ba(OH)2.
Weak acids
HF, HCN, CH3COOH, etc.
Weak bases
NH3, CH3NH2, etc.
Phases solubility Rules
Solids are more soluble at higher temperatures
Gases are more soluble at lower temperatures
Gases are more soluble at higher temperatures
Spectrophotometry
A method that measures how much a chemical substance absorbs light by measuring the intensity of light as a beam of light passes through a sample solution. A spectrophotomer measures how much light is sent into the solution and how much light comes out.
Beer’s law
States that light absorption is directly proportional to path length and concentration of solution.
A = Elc
A= absorbance
E= molar absorptivity
l = path length
c = concentration of solution
Like dissolves like
Polar solvents dissolve polar solutes
Non-polar solvents dissolve non-polar solutes
Polar and non-polar do NOT dissolve in each other.
Heterogenous mixtures
Have particles distributed non-uniformly. They can be physicallly seperated and have visually distinguishable components.
Homogenus mixtures
Have their particles distributed uniformly. These mixtures cannot be physically seperated and the individual components cannot be identified.
Molarity
M= moles of solute / liters of solution
Molality
m = moles of solute / kilograms of solvent
Dilution formula
M1 V1 = M2 V2
M is molarity
V is volume
Normality
N = n x M
n = number of equivalents (how many H+ it takes/dissociates)
M = molarity
Colligative properties
Depend on the concentration of solute molecules or ions, but not on the identity of the solute itself.
Vapor-pressure depression
Boiling point elevation
Freezing point depression
Osmotic pressure
Non-colligative properties
Depend on the identity of the dissolved species and solvent.
Surface tension
Viscosity (measure of the fluid’s resistance to flow)
Solubilty
Voltality (how easily a substance evaporates)
Color and density
Boiling point
Point where the vapor pressure equals the atmospheric pressure. When elevation increases, vapor pressure decreases and boiling point decreases. As elevation descreases, atmoshperic pressure increases and boiling point increases.
Vapor pressure depression
The vapor pressure of a pure solvent is greater than the vapor pressure of a solution containing non-volatile solutes. As vapor pressure increases, boiling pressure decreases. If a solution has a dissolved solute, it lowers the vapor pressure.
Raoult’s law
Use to calculate the new vapor pressure after a solute has been added.
PA= XAPA∘
PA= vapor pressure of the solution after the solute has been added
XA = mole fraction of the solvent
PA∘ = pure vapor pressure of solvent
Boiling point elevation
When a non-volatile solute is added to a solution, it increases the solution’s boiling point.
ΔTb = kbim