The amount of iron in a meteorite is determined by a redox titration using KMnO4 as the titrant. A 0.4185-g sample is dissolved in acid and the liberated Fe3+ quantitatively reduced to Fe2+ using a Walden reductor. Titrating with 0.02500 M KMnO4 requires 41.27 mL to reach the endpoint. Determine the %w/w Fe2O3 in the sample of meteorite.
Solution:
Balanced chemical equation for the titration reaction:
5Fe2+ + MnO4− + 8H+ → 5Fe3+ + Mn2+ + 4H2O
By stoichiometry, n(Fe2+)/5 = n(MnO4−)
n(MnO4−) = C(MnO4−) × V(MnO4−) = 0.02500 M × 0.04127 L = 0.00103175 mol
Therefore,
n(Fe2+) = 5 × n(MnO4−) = 5 × 0.00103175 mol = 0.00515875 mol
Fe2O3 → 2Fe3+ → 2Fe2+
According to the scheme above: n(Fe2O3) = n(Fe2+)/2
n(Fe2O3) = n(Fe2+) / 2 = 0.00515875 mol / 2 = 0.002579 mol
The molar mass of Fe2O3 is 159.69 g/mol.
Therefore,
(0.002579 mol Fe2O3) × (159.69 g Fe2O3 / 1 mol Fe2O3) = 0.4119 g Fe2O3
Mass of Fe2O3 = 0.4119 g
%w/wFe2O3 = (mass of Fe2O3 / mass of sample) × 100%
%w/wFe2O3 = (0.4119 g / 0.4185 g) × 100% = 98.42%
%w/wFe2O3 = 98.42%
Answer: %w/wFe2O3 = 98.42%
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