}}formation of solutions!}}
when dissolved!
three ways to dissolve a solid more quickly!
stir: (shake, agitate)
decrease particle size: (grind)
heat:
}}solubility}}[mass (or number of mols) of solute / volume of solution/solvent]
factors affecting solubility
temperature
pressure
solids dissolve easily in lower pressures
gases dissolve easily in higher pressures
}}saturation}}
**use solubility chart/curve
saturated: solution where is has the max amount of solute at a particular temperature
unsaturated: solution with less than the max amount of solute
supersaturated: solution with more than the maximum amount of solute
difference between supersaturated solution and max amount of solution is what precipitates out
}}concentration}}
expresses how much solute is dissolved in solvent
}}molarity (M)}}
moles of solute (n) per liter of solution (V)
M = (n/v) = (moles solute/liters of solution)
**dependent on temperature because volume of solution would change slightly
}}molality (cursive small ‘m‘)}}
moles solute per kilogram of solvent
m = (moles of solute / kg of solvent)
**not dependent on temperature!
}}parts per million (ppm) and parts per billion (ppb)}}
used for expressing very small concentrations, particularly for containments in environment
ppm = [ mass of solute (g) / vol of solution (mL)] * 10^6 (million)
ppb = [mass of solute (g) / vol of solution (mL)] * 10^9 (billion)
dilution
a dilute solute can be made by adding more solvent to a concentrated solution
serial dilution!
}}colligative properties}}
lower vapor pressure
solute particles inhibit solvent from escaping as gas
boiling point elevation
solute particles make it more difficult for solvent to escape as gas
more energy needs to escape → higher temperature to boil
determining ΔBP: ΔT = (i)(Kb)(m)
ΔBP - change in temperature, not new boiling point
i - # of disassociated particles
VAN’T HOFF FACTOR
i for all molecular compounds equals one!!
Kb - boiling constant, unique for each constant
m - molality: moles solute/kg solven
freezing point depression
solute particles prevent pure solvent from forming
cold temp needed to form solid
determining ΔFP: ΔT = (i)(Kf)(m)
ΔT - change in freezing point
i - # of particles
Kf - freezing constant
m - molality
osmotic pressure
osmosis: the movement of H2O through semi-permeable membrane
increases as the difference in concentration increases
* applying force to stop water from moving across the membrane