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About Rot
Decomposition or rot is the process by which dead organic substances are broken down into simpler organic or inorganic situation such as carbon dioxide, water, simple sugars and mineral salts. The process is a part of the nutrient cycle and is indispensable for recycling the finite matter that occupies physical heavens in the biosphere. Bodies of busy organisms begin to decompose gruffly after death. Animals, such as earthworms, also support decompose the organic materials. Organisms that accomplish this are known as decomposers or detritivores. Although no two organisms decompose in the thesame way, they anything undergo the similar sequential stages of decomposition. The science which studies decomposition is generally referred to as taphonomy from the Greek word taphos, meaning tomb. Decomposition can also be a gradual process for organisms that have extended periods of dormancy.
One can differentiate abiotic decomposition from biotic decomposition (biodegradation). The former means “the degradation of a substance by chemical or inborn processes”, e.g., hydrolysis; the latter means “the metabolic breakdown of materials into simpler components by thriving organisms”, typically by microorganisms.
