Question:

Laterite soil is rich in

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Laterization is a soil-forming process characterized by silica removal (desilication) and the accumulation of iron and aluminum oxides.
  • Ca
  • Fe
  • C
  • Cu
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The Correct Option is B

Solution and Explanation



Step 1: Understanding the Concept:

Laterite soils form under high temperatures and heavy, seasonal rainfall.
This climate promotes intense chemical weathering and leaching of mobile elements.

Step 2: Detailed Explanation:

- High rainfall causes silica ($\text{SiO}_2$) and basic cations ($\text{Ca}^{2+}$, $\text{Mg}^{2+}$, $\text{K}^+$) to leach deep into the soil profile.
- Less mobile sesquioxides, primarily oxides and hydroxides of iron ($\text{Fe}$) and aluminum ($\text{Al}$), accumulate in the upper horizons.
- This oxide accumulation gives laterite soils their characteristic reddish-brown color and high iron content.

Step 3: Final Answer:

Laterite soils are rich in iron ($\text{Fe}$).
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