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Iron toxicity

Iron toxicity

Description

Systematic position and nature: Iron toxicity is not an infectious disease but a physiological disorder caused by abiotic stress. It results from the excessive uptake of ferrous iron (Fe2+) by plant roots, leading to internal toxicity. Since it is not caused by a biological agent, it is categorized as a nutritional imbalance induced by specific soil chemical conditions.

Affected crops and symptoms: The disorder is most prevalent in waterlogged crops, especially rice. The hallmark symptom is known as "bronzing," characterized by the development of orange-brown spots on the leaves, which eventually turn dark brown. Root systems often appear stunted, dark, or decayed, significantly reducing the plant's capacity to absorb nutrients and water.

Biology and environmental conditions: The phenomenon occurs predominantly in waterlogged, acidic soils with low redox potential. In such environments, insoluble iron (Fe3+) is reduced to its soluble and toxic divalent form (Fe2+). This process is exacerbated by high organic matter content and prolonged flooding, which depletes dissolved oxygen and facilitates the accumulation of toxic levels of iron in the soil solution.

Economic importance: The damage caused by iron toxicity is significant, as it leads to severe growth inhibition and yield loss. By interfering with the uptake of essential nutrients like potassium, phosphorus, and zinc, iron toxicity weakens the plant's defense mechanisms. In severe outbreaks, yield reductions in rice can exceed 50%, making it a major limiting factor in wetland agricultural systems.

Protection and control measures: Management strategies focus on improving soil conditions and enhancing plant tolerance:

  • Liming of acidic soils to increase pH and decrease iron solubility.
  • Improving drainage systems to prevent long-term anaerobic conditions in the root zone.
  • Application of balanced fertilizers, particularly potassium, to help maintain plant vigor.
  • Selection of tolerant crop cultivars that can oxidize iron at the root surface or restrict its transport to shoots.
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