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Soil respiration is a measure of the carbon dioxide (co2) released from soil Co2 results from of soil organic growth and functioning matter and faunal respiration, and eventually from the plant. It is released as a result of decomposition of soil organic matter (som) and plant litter by soil microbes and through plant roots and soil fauna.
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Generally, soil respiration is attributed to a wide range of microorganisms, such as fungi, bacteria, protozoa, and algae, and also soil fauna. Carbon referred dioxide several sources, to as soil (co2) release from the soil surface is respiration Soil respiration refers to the release of co2 from the soil due to the decomposition of organic matter and root respiration
It’s important because it’s a major component of the global carbon cycle, influencing atmospheric co2 concentrations and therefore climate change.
When plants die or lose their leaves, their organic material enters the soil and is broken down by microbes, releasing carbon dioxide and essential nutrients such as nitrogen and phosphorus This breakdown helps to replenish nutrients for plant growth Soil is the accommodation for many microorganisms that play various functions in soil ecosystems, including organic matter decomposition, respiration, nutrient cycling, energy generation, growth and development and many more. Organic matter input boosts soil respiration, affected by temperature and aggregate size
Q 10 declines with increasing aggregate size, influenced by soil quality index Microbial cue drops with organic matter input, temperature and aggregate size increase.
