Decomposition Simplified Revision Notes for Scottish Highers Geography
Revision notes with simplified explanations to understand Decomposition quickly and effectively.
Learn about Soil Formation for your Scottish Highers Geography Exam. This Revision Note includes a summary of Soil Formation for easy recall in your Geography exam
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Discuss Decomposition.
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.
Moisture: Adequate moisture is essential for decomposition.
Oxygen: Decomposers require oxygen for their metabolic processes.
Discuss Decomposition.
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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