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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 business such as carbon dioxide, water, simple sugars and mineral salts. The process is a part of the nutrient cycle and is essential for recycling the finite business that occupies physical look in the biosphere. Bodies of busy organisms start to decompose immediately after death. Animals, such as earthworms, also help decompose the organic materials. Organisms that get this are known as decomposers or detritivores. Although no two organisms decompose in the similar way, they anything undergo the same 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 monster processes”, e.g., hydrolysis; the latter means “the metabolic breakdown of materials into simpler components by successful organisms”, typically by microorganisms.
