Colligative Properties of Nonelectrolyte Solutions
Transcript of Colligative Properties of Nonelectrolyte Solutions
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Colligative Properties ofNonelectrolyte SolutionsColligative Properties ofNonelectrolyte Solutions
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Colligative Properties
Depends only on number of particles of asolute in solution and not on the natureof the solute
Boiling point elevation
Vapor pressure lowering
Freezing-point depressing
Osmotic Pressure
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Vapor Pressure
The pressure exerted by a vapor inequilibrium with its liquid
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volatile
nonvolatile
Does not have a measurable vaporpressure
having a measurable vapor pressure
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Vapor pressure lowering
The vapor pressure of a solution containing anonvolatile solute is always less than that ofthe pure solvent.
the nonvolatile solute lowers the number ofvolatile solvent molecules at the surface ofthe solution
less opportunity for solvent molecules toescape into the gas phase
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The solute dilutes the solvent
Vapor pressure lowering
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Vapor pressure of water-mannitol solutions
17.2
17.6
17.5
17.4
17.3
.0 .5 .75 1.0.25
++
++
++
+Vapor pressure(mm Hg )
Moles mannitol / 1000 g water
At 25°C
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Raoult’s LawRaoult’s Law
Psolution = (X solvent ) ( P ° solvent )
The vapor pressure of the solution isproportional to the mole fraction of the solventin the solution.
Vapor pressuresolution
mole fraction ofthe solvent
Vapor pressureof pure solvent
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Raoult’s Law represents an equationof a straight line
Psolution = X solvent P ° solvent
y = x m + b = 0
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Ideal solution
Vaporpressure
XA
0.0 0.25 0.50 0.75 1. 0
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Example
Calculate the vapor pressure of a solution of 0.250mol of sucrose in 1.100 mol of water at 50 ° C. Thevapor pressure of pure water at 50 ° C is 92.5torr.
1.100 mol H2O 0.250 mol sucrose+
1.100 mol H2OXA = = 0.815
= ( 0.815 ) ( 92.5 torr ) = 75.4 torr
PA = XA P ° APA = XA P ° A
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Example
Adding 20g of urea to 125g of water at 25 ° C, atemperature at which water has a vapor pressure of23.76 torr.The vapor pressure of the solution is 22.67torr.Calculate the molar mass of urea.
P °H2O
X =H2O
Psoln=
23.76 torr
22.67 torr0.9541=
125g H2O x18g H2O
1 mol H2O6.94 mol H2O=
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mol H2O mol urea+
mol H2OX =H2O 6.94 mol urea+
6.94= 0.9541=
.335 mol urea
20g urea= 59.7g/mol
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If both components of the solution arevolatile,
PT = PA + PBDalton’s law of
partial pressures
PA = XA P ° Apartial pressures
component A
PB = XB P ° Bpartial pressures
component B
the vapor pressure of the solution isthe sum of the individual partial pressures
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Ideal solution
Defined as one that obeys Raoult’s Law
No attractive forces between solute andsolvent
DH ° (solution ) = 0
Ideal behavior is most closely approachedwhen the solution is dilute
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Ideal solution
Vaporpressure
PT = PA + PB
PBPA XA
0.0 0.25 0.50 0.75 1. 0
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Negative Deviation
a solution with a lower than expected vaporpressure
attractive forces between solute and solvent
- DH ° (solution )
(Raoult’s Law)
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Vaporpressure
PT = PA + PB
PBPA XA
0.0 0.25 0.50 0.75 1. 0
Negative Deviation
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Positive Deviation
liquid-liquid solutions with higher thanexpected vapor pressures
weaker solute solvent interactions than thepure solvent
+ DH ° (solution )
(Raoult’s Law)
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Vaporpressure
PT = PA + PB
PBPA XA
0.0 0.25 0.50 0.75 1. 0
Positive Deviation
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Since its vapor pressure at a particulartemperature is depressed, the boiling point of asubstance must be higher.
Boiling-point elevation andfreezing-point depression
Adding a solute to a solvent interferes with thesolvents ability to go into the solid phase. Thuslowering the temperature at which the solventfreezes.
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liquid
solid
gas
100 ° C
760mmHg
P
0 ° C
Phase diagram H2O
T
1 atm
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Boiling-point elevationBoiling-point elevation
K b is called the molal boiling-point elevationconstant
Elevation in boiling point is proportional to themolal concentration of the solute m
DT = K b msolute
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Boiling pointwhen the vapor pressure of a liquid is equal to thesurrounding atmospheric pressure
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Boiling point ElevationAs a nonvolatile solute is added the vaporpressure of the solvent is lowered
i.e. solvent moleculesneed more kineticenergy to escape intothe gas phase
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Freezing-point depressionFreezing-point depression
K f is called the molal freezing -point depressionconstant
Depression in freezing is proportional to themolal concentration of the solute m
DT = K f msolute
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an equilibrium is established between the solidphase and the liquid phase
Freezing-point
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the presence of a solute lowers the rate at whichmolecules return to the solid state
Freezing-point depression
a new equilibrium isestablished between thesolid phase and theliquid phase at a lowertemperature
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Calculate the boiling point of a solution of 0.0150 molanthracene (which is nonvolatile) in 45.0 g of toluene ( Kb fortoluene is 3.33°C kg / mol ) ; the normal boiling point oftoluene is 110.63 °C.
Boiling-point elevationBoiling-point elevation
DT = K b msoluteDT = K b msolute
m =Mol sol
Kg solv =
0.333 mol
kg
=0.333 mol
kgx
3.33°C kg
molDT = 1.11°
110.63 ° C 1.11° = 111.74° C+
= x103 g
1 kg
0.0150 mol anth.
45.0 g tolu.
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Calculate the freezing point of a solution of 0.047 mollactose(a sugar) in 25.0 g of water( Kf for water is 1.86°C kg /mol ).
Freezing point depressionFreezing point depression
DT = K f msoluteDT = K f msolute
m =Mol sol
Kg solv =
0.047 mol lac.
25.0 g H2Ox
103 g
1 kg=
1.88 mol
kg
=1.88 mol
kgx
1.86°C kg
molDT = 3.50°
0° C 3.50° = -3.50 ° C-
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Osmotic Pressure (p)Osmotic Pressure (p)
allows solvent molecules to passthrough but not solute molecules
Semipermeable membrane:
osmosis:The passing of solvent moleculesacross a semipermeable membrane
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(M) molarity of the solute
p = MRT
Osmotic Pressure (p)Osmotic Pressure (p)
the pressure required to stop osmosis
(R) gas law constant(T) kelvin temperature
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Porous Barrier
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the rate of transfer is greater from solvent to solutionthan from solution to solvent
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OsmoticPressure (p)
at equilibrium the rate of solvent transfer is the same inboth directions
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1.0x10-3 g of protein is dissolved in 1.0 ml of water.Theosmotic pressure of this solution was found to be 1.12 torr at25.0 °C. Calculate the molar mass of the protein (density ofthe solution is 1 g/L )
=1.47 x 10-3 atm
(0.0821 L atm/ K mol)(298K)M
Osmotic Pressure (p)Osmotic Pressure (p)
p = =x1 atm
760 torr1.12 torr 1.47 x 10-3 atm
M = p /RT
= 6.01 x 10-5 mol/L
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d =1 g
L
1L
6.01 x 10-5 molx
1 g
6.01 x 10-5 mol=
1 g
6.01 x 10-5 mol= 1.66 x 104 g/mol
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Dialysis
Isotonic solutionshave identical osmoticpressures
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Dialysis
Hypertonic solutionsHigher osmotic pressure
Hypotonic solutionslower osmotic pressure
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Dialysis
A newequilibriumestablished