The carbon cycle. Principles and meaning
In the biosphere of our planet there are manycomplex processes caused by the vital activity of organisms, human exposure and evolutionary changes occurring in the depth of the interior and in the depths of the oceans. The main one is the carbon cycle. Without it, life on earth is impossible.
The scheme of the carbon cycle will allow more complete representation of this process, consisting of two stages:
- Assimilation of carbon dioxide (CO2) plants, microscopic living organisms and the subsequent transformation of it into more complex basic chemical compounds (fats, carbohydrates, proteins).
- The return of carbon dioxide to the atmosphere through the breathing of living beings and other ways.
However, the carbon cycle is moredifficult process. So, after the death of organisms, some of them are processed by bacteria and actually returns to the atmosphere in a relatively short time. But some of the remains turn into a dead organic mass.
Separately, I want to focus on the process of returning CO2 in the carbon cycle.
Fats. The splitting of fats of different origin is possible due to the participation in this process of microorganisms possessing enzymes aimed at cleavage of this compound. As a result, glycerol and higher fatty acids are formed. Glycerin decomposes into pyruvic acid (PVC). It, depending on the conditions, will turn into water, acid or alcohol, and a carbon molecule will be released into the air.
Carbohydrates. These substances are the main carriers of cellulose, which
In connection with the fact that all processes are not the same in terms of their timing, two types of cycling of this substance are distinguished in the biosphere:
- Geological (formation of minerals) - can be estimated in thousands and millions of years.
- Biological (death and decay of plants and animals) is a very active process, which can take from several days to several years.
Of course, the description presented here is very superficial and does not reflect the whole essence of the chemical and other processes, thanks to which the carbon cycle is supported on the planet.