Worked solution
Part (a): Writing the Kpc expression
The partition coefficient of iodine between hexane and water is defined as the ratio of its equilibrium concentration in hexane to its equilibrium concentration in water:
Kpc=[I2(aq)][I2(hexane)]
Part (b): Calculating Kpc
Substituting the given equilibrium concentrations:
Kpc=2.50×10−42.05×10−2=82.0
(Check: recomputing independently, 2.05÷2.50=0.820, and 0.820×10(−2)−(−4)=0.820×102=82.0. Consistent.)
Part (c): New equilibrium concentration after adding hexane
Total amount of iodine. Before shaking with hexane, all the iodine is in the aqueous layer:
n(I2)total=1.00×10−3×100025.0=2.50×10−5 mol
Setting up the balance. Let the new equilibrium concentration in the aqueous layer be caq. Since Kpc=82.0 is unchanged, the equilibrium concentration in hexane is chex=82.0caq. The total amount of iodine is conserved between the two layers, of volumes Vaq=25.0 cm3=0.0250 dm3 and Vhex=10.0 cm3=0.0100 dm3:
n(I2)total=caqVaq+chexVhex=caq(0.0250)+82.0caq(0.0100)
2.50×10−5=caq(0.0250+0.820)=caq(0.845)
Solving for caq:
caq=0.8452.50×10−5=2.959×10−5 mol dm−3 ⇒ [I2(aq)]=2.96×10−5 mol dm−3 (3 s.f.)
(Check: chex=82.0×2.959×10−5=2.426×10−3 mol dm−3. Moles: naq=2.959×10−5×0.0250=7.40×10−7 mol; nhex=2.426×10−3×0.0100=2.426×10−5 mol. Sum =7.40×10−7+2.426×10−5=2.500×10−5 mol, matching the total from above, consistent. As expected, caq is far smaller than the original 1.00×10−3 mol dm−3, since Kpc=82.0 strongly favours the hexane layer.)
Final answers
- (a) Kpc=[I2(aq)][I2(hexane)]
- (b) Kpc=82.0
- (c) [I2(aq)]=2.96×10−5 mol dm−3