Decomposition – Class 12 | Chapter – 14 | Biology Short Notes Series PDF

Decomposition: It is the process by which dead organic matter is broken down by decomposers, such as bacteria and fungi, into simpler inorganic compounds. This process is also known as decay, and it plays a critical role in the ecosystem by returning nutrients, such as carbon, nitrogen, and phosphorus, to the soil for reuse by plants and other organisms.

The process can be divided into several stages, including death and decay, consumption by decomposers, absorption of nutrients, release of nutrients, and reuse of nutrients. During this process, the dead organic matter is broken down into smaller pieces, which are more easily consumed by decomposers. The decomposers then use the nutrients released during the decomposition process for their own growth and reproduction, releasing some of the nutrients back into the soil for reuse by plants and other organisms.

This is a vital part of the ecosystem, as it helps to maintain the balance of nutrients and support the food chain. It is also important for regulating the Earth’s climate, as the decomposition of organic matter releases carbon dioxide into the atmosphere. The decomposition cycle is a continuous process that helps to support the health and sustainability of the ecosystem, playing a key role in the balance of life on Earth.

Types of Decomposition

  • Aerobic decomposition: It occurs in the presence of oxygen and is carried out by aerobic bacteria and fungi. It is a faster and more efficient process than anaerobic decomposition, producing carbon dioxide and water as by-products.

  • Anaerobic decomposition: It occurs in the absence of oxygen and is carried out by anaerobic bacteria. It is a slower and less efficient process than aerobic decomposition, producing methane and other by-products, such as carbon dioxide and hydrogen sulfide.

Factors influencing Decomposition

  • Climate: Decomposition is affected by temperature, moisture, and sunlight, with warmer and moister conditions generally promoting faster decomposition rates.

  • Nutrient availability: The availability of essential nutrients, such as nitrogen and phosphorus, can impact the rate of decomposition. A lack of these nutrients can slow down the decomposition process.
  • Microorganisms: The type and abundance of decomposers, such as bacteria and fungi, can influence the rate and process of decomposition. Some decomposers are more efficient at breaking down certain types of organic matter than others.
  • Chemical composition of organic matter: The chemical composition of the organic matter, including its carbon-to-nitrogen ratio, can impact the rate of decomposition. A higher carbon-to-nitrogen ratio can slow down the decomposition process.
  • Soil type: Soil type, including its physical structure, pH, and nutrient content, can influence the rate and process of decomposition.
  • Protective structures: Certain structures, such as lignin and cellulose in plant material, can slow down the decomposition process.
  • Land use: Land use, such as agriculture and urbanization, can impact the rate and process of decomposition through the use of pesticides and other chemicals, changes in soil structure, and alterations to the local climate.


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By Team Learning Mantras