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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 matter such as carbon dioxide, water, simple sugars and mineral salts. The process is a part of the nutrient cycle and is valuable for recycling the finite thing that occupies physical broadcast in the biosphere. Bodies of active organisms begin to decompose shortly after death. Animals, such as earthworms, also support decompose the organic materials. Organisms that attain this are known as decomposers or detritivores. Although no two organisms decompose in the similar way, they everything undergo the thesame sequential stages of decomposition. The science which studies decomposition is generally referred to as taphonomy from the Greek word taphos, meaning tomb. Decomposition can as well as 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 being processes”, e.g., hydrolysis; the latter means “the metabolic assay of materials into simpler components by flourishing organisms”, typically by microorganisms.
