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Decomposition Simplified Revision Notes

Revision notes with simplified explanations to understand Decomposition quickly and effectively.

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Introduction

  • Soil formation is a complex process involving the breakdown of rocks, sediments, and organic matter.
  • Decomposition is a key component of this process, where organic material transforms into soil.

Weathering

  • Weathering is the physical and chemical breakdown of rocks and sediments.
  • Physical weathering includes processes like freezing and thawing, which break rocks into smaller pieces.
  • Chemical weathering involves reactions that alter the mineral composition of rocks.

Decomposition

  • Decomposition is the breakdown of organic matter (such as leaves, plants, and dead animals) into simpler substances.
  • It is primarily driven by microorganisms like bacteria and fungi.
  • Decomposers break down organic matter into humus, a dark, organic-rich material.

Importance of Decomposition

  • Decomposition enriches the soil with nutrients and organic material.
  • It improves soil structure, aeration, and water-holding capacity.
  • Decomposition also contributes to the carbon cycle, releasing carbon dioxide back into the atmosphere.

Factors Affecting Decomposition

  • Temperature: Higher temperatures accelerate decomposition.
  • Moisture: Adequate moisture is essential for decomposition.
  • Oxygen: Decomposers require oxygen for their metabolic processes.

Discuss Decomposition.

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Summary

  • Soil formation involves the breakdown of rocks, sediments, and organic matter.
  • Decomposition, driven by microorganisms, transforms organic material into humus, enriching the soil.
  • Factors like temperature, moisture, and oxygen influence the rate of decomposition.
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