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The amount of iron in a meteorite was determined by a redox titration using KMnO 4 as the titrant. A 0 . 7 6 5

The amount of iron in a meteorite was determined by a redox titration using KMnO4 as the titrant. A 0.765 g sample was dissolved in acid and the liberated Fe3+ quantitatively reduced to Fe2+. Titrating with 0.023 M KMnO4 requires 49.19 ml to reach the end point.
Unbalance reaction: Fe2++ MnO4--> Fe3++ Mn2+.
Determine the % w/w Fe2O3 in the meteorite

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