Carbon, hydrogen, oxygen and nitrogen is the most common element in all living organisms. Nitrogen is a constituent of amino acids, proteins, hormones, chlorophylls and vitamins. It is also the most abundant gas in the atmosphere. However, plants can not use this nitrogen directly and use the nitrogen cycle to produce usable nitrogen. Let us learn more about its definition, steps with the help of a nitrogen cycle flowchart, reactions and significance.
What is Nitrogen Cycle?
“Nitrogen Cycle is a process that converts nitrogen into many forms by continuously passing it from the atmosphere to the soil then, to the organisms and finally sends it back into the atmosphere.”
It is a bio-geochemical process, that helps in converting atmospheric nitrogen into usable nitrogen for plants. Furthermore, plants compete with microbes present in the soil because of the limited availability of nitrogen. Thus, nitrogen is a limiting nutrient for natural and agricultural ecosystems.
Process of Nitrogen Cycle – Steps
So, as we can see from the nitrogen cycle flowchart, it consists of several steps. Let us discuss them in detail here.
Step 1: Nitrogen Fixation
“Nitrogen-fixation is the process of conversion of nitrogen to ammonia.”
As we know, nitrogen exists as a diatomic molecule having two nitrogen atoms linked by a strong triple covalent bond i.e. N ≡ N. The reaction that takes place is:
N2 + 8 H+ + 8 e− → 2 NH3 + H2
Only certain prokaryotic organisms are capable of fixing nitrogen because of the presence of enzyme nitrogenase in them. Such micro-organisms are known as N2-fixers or diazotrophs. Since micro-organisms fix nitrogen, it is also known as biological nitrogen fixation.
Furthermore, non-biological nitrogen fixation deals with the nitrogen fixation done through non-biological methods like lightening, combustion, ultraviolet radiations, automobile exhausts, etc.
There are two groups of organisms that help in this process
- Symbiotic Nitrogen fixer and
- Non-Symbiotic Nitrogen fixer.
Symbiotic Nitrogen Fixers:
These are the bacteria living symbiotically in root nodules (small outgrowths on roots) of legume plants that can fix atmospheric nitrogen and make it available for the plants. For example, Rhizobium and Frankia.
Non-symbiotic Nitrogen Fixers:
These are free-living microorganisms that fix atmospheric nitrogen into ammonia. For example, Azotobacter, Beijerinekia, Clostridium, Derxia, etc. [Tip to remember: A B C D = Azotobacter, Beijerinekia, Clostridium, Derxia]
Step 2: Nitrification
“Nitrification is the process of biological formation of nitrate and nitrite from ammonia.”
It takes place in two steps:
- Oxidation of ammonia to nitrite by the bacteria Nitrosomonas and/or Nitrococcus. That is,
- 2 NH4+ + 3 O2 → 2 NO2– + 2 H2O + 4 H+
- Further oxidation of nitrite to nitrate with the help of the bacterium Nitrobacter. That is,
- 2 NO2– + O2 → 2 NO3–
Nitrification is a reductive process. It is an important step because the transformation of NH4+ ion into NO3– ion results in the shift in charge from positive (+ve) to negative (-ve). The positively charged ion tends to bind with negatively charged particles in the soil. Whereas, the negatively charged NO3– ion tends to freely migrate in soil water so that, plants can radially take up nitrate ion by roots for using it in organic compounds.
Step 3: Ammonification
“Ammonification is the process of decomposition of organic nitrogen of dead plants and animals into ammonia.”
Bacterias like Pseudomonas, Bacillus, clostridium; fungi like Alternaria, Aspergillus, Mucor, Penicillium, and Actinomycetes like Streptomyces are responsible for converting organic nitrogen compounds into ammonia.
The reaction is: NH3 → NH4+
The breakdown starts with detritus i.e. dead plants and animals, where proteins are decomposed into amino acids by enzyme proteases. These amino acids further break down to ammonia (NH3). This ammonia is finally converted to ammonium (NH4+). However, some of the ammonia volatilizes and goes back into the atmosphere.
Step 4: De-nitrification
“De-nitrification is the biological conversion of nitrite and nitrate into nitrous oxide or molecular nitrogen gas.”
It is fundamentally, the reduction of nitrate present in the soil to nitrogen. Firstly, nitrate reduces to nitrite which then reduces to nitric oxide, then nitric oxide reduces to nitrous oxide, and finally to molecular nitrogen.
Furthermore, de-nitrification causes the loss of soil nitrogen into the atmosphere. This process is called the volatilization of nitrogen.
Some of the denitrifying bacteria are Pseudomonas denitrificans, Bacillus licheniformis, Thiobacillus denitrificans, Hypomicrobium, Chromobacterium, etc. Also, these denitrifying bacteria are anaerobic in nature.
Significance of Nitrogen Cycle
The nitrogen cycle is quite important for plants and microorganisms present in the soil. Such as,
- It helps plants to synthesise chlorophyll from the nitrogen compounds.
- It helps in capturing and converting inert nitrogen gas into a usable form for the plants.
- Ammonification i.e. the third step of the nitrogen cycle, helps the bacteria in decomposing the animal and plant matter, which in turn, helps to clean up the environment.
- The discharge of nitrates and nitrites, during the cyce, helps in enriching the soil with the necessary nutrients that benefits cultivation and agriculture.
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