Microbial Decomposition Essay

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The rates of microbial decomposition, amount of organic material inputs, and the capability organic matter retain in the soil influenced the accumulation of SOM. Extension rate of decomposition is depending on the quality of the plant residue. Simple sugars content labile C compounds degrade rapidly to CO2 meanwhile lignin is more complicated to degrade. Most microorganisms do not have the capability to degrade lignin completely. The incomplete degradation products will initially promote to soil organic matter. Decomposition ability usually showed by C:N ratio while Lignin:N ratio used to appraise organic matter decomposition. Lows decomposition and immobilizes N; show by reading ratio more than 30 while below 20, N will freely moves and lets the microorganism to proceed degradation.

Decomposition of plant material and soil organic matter by microorganisms is influenced by climate. Reported by Linn et al., 1984, temperature and soil water content are important aspects in microbial activity. Microbial activity doubles (Q10 = 2) for every 10oC temperature increase and optimal microbial activity happen at near “field …show more content…

It affects the efficiency of soil aggregation which a combination between soil particles and cation. SOC is the carbon from organic matter. Aggregate stability is very closely with the organic carbon content. The organic matter appears to be a predominant indicator of aggregate stability. SOC is assumed to stabilize aggregate against disruptive process by two major actions. First, organic matter increase the cohesion of aggregate, through the binding of mineral particles by organic polymer or through the physical enmeshment of particles by fine roots, fungal hyphae or cynobacteria (Tisdall and Oedes, 1982). Second, organic matters decrease the wettability of aggregate by slowing their rate of wetting and thus extent of slaking (Chenu et al.,

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