As the acidic, iron-rich water moves along the streams, an interesting chemical transformation occurs. The ferrous iron \((\text{Fe}^{2+})\), initially released from sulfide oxidation, can further undergo oxidation. In the presence of water and oxygen, ferrous iron changes to ferric iron \((\text{Fe}^{3+})\).
This transformation is represented by:\[ \text{4Fe}^{2+} + \text{O}_2 + 10\text{H}_2\text{O} \rightarrow 4\text{Fe(OH)}_3 + 8\text{H}⁺. \]
Ferric iron subsequently reacts with water to form insoluble iron hydroxide \((\text{Fe(OH)}_3)\). This compound is known commonly in the field as "yellow boy" because of its distinct red-brown color.
- Sediment deposition: As the stream flows, this iron hydroxide precipitates and settles on riverbeds, forming the observed red-brown layers.
- Environmental impact: These deposits can affect aquatic life, clogging habitats and altering the natural flow of nutrients and water through the area.