In
previous posts we discussed how the organic carbon is transferred to the ground
and what exactly happens in the organic matter during the decomposition procedure.
But how fast is it decomposed?
The
organic matter influences the microbial activity in the soil, acting as a carbon
source for the microbes (Agren and Bosatta, 1996).As the organic matter is transferred
from the plants to the soil, the different substances are decomposed with
different speed depending on their structures (Stockmann et al., 2011). For example, leafs are decomposed
faster than the wood.
Many
studies (Meentemeyer, 1978; Parton et al., 2007; Melillo et al., 1982) have concluded that the main
factors contribute in the decomposition rate, are:
- Climate
- Humidity
- Microbiology of the soil
- Quality of the organic matter
The
climate and the humidity of the soil affect the microorganisms, thus the
decomposition of the organic matter. In general, the quality of the organic matter can be
characterized by the C/N (Carbon/Nitrogen) ratio. To be more specific, the higher
the C/N ratio, the lower the decomposition rate of the organic matter (Melillo et al., 1982; Gupta and Germida, 1988). That shows the importance of the relation
between the nitrogen and the carbon cycle, giving the ‘title’ of the limiting
factor for the microbial activity.
The
increase of the CO2 emissions helps the greenhouse effect rising the
global temperature (see 3rd post-Human influence in the Atmosphere!).
The decomposition of the soil carbon is affected by the temperature because
there is a positive feedback to the microbial activity due to temperature
increase. This means that the terrestrial carbon is released back to the
atmosphere (Stockmann et al., 2011).
A general
view of the carbon movements in the terrestrial ecosystem is illustrated below:
See
you very soon!
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