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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 issue such as carbon dioxide, water, simple sugars and mineral salts. The process is a allocation of the nutrient cycle and is essential for recycling the finite matter that occupies physical manner in the biosphere. Bodies of booming organisms begin to decompose sharply after death. Animals, such as earthworms, also put in the works to decompose the organic materials. Organisms that complete this are known as decomposers or detritivores. Although no two organisms decompose in the similar way, they all 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 afterward 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 psychotherapy of materials into simpler components by vivacious organisms”, typically by microorganisms.
