Abstract
The decomposition of H2O2 by ferric perchlorate was investigated using parallel titrimetric and spectrophotometric measurements. During the decomposition complexes are formed between HO2- and Fe3+. The results can be represented by the following mechanism, involving two complexes: Fe3+ + HO2- ⇌ k2 k1 {Fe3+HO2-} I {Fe3+HO2-}I → k3 {Fe3+HO2-}II {Fe 3+HO2-}II + H2O 2 → k4 products. The products are Fe3+, OH-, H2O and O2. At high [H2O 2]/[Fe3+] ratios (300 to 10) the kinetic results are satisfactorily represented by a mechanism involving the first complex only. At lower ratios (4 to 0.2) the second complex too becomes kinetically important.
| Original language | English |
|---|---|
| Pages (from-to) | 959-973 |
| Number of pages | 15 |
| Journal | Transactions of the Faraday Society |
| Volume | 55 |
| DOIs | |
| State | Published - 1959 |
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