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NEET Biology
Nitrogen Assimilation

Nitrogen Assimilation

Nitrogen assimilation refers to the process by which living organisms, particularly plants and microorganisms, take up and incorporate nitrogen from the environment into organic compounds. Nitrogen is an essential element for the synthesis of various biomolecules, including proteins, nucleic acids, and other cellular components.

In the context of plants, nitrogen assimilation primarily involves the uptake of inorganic nitrogen from the soil in the form of nitrate (NO₃⁻) or ammonium (NH₄⁺). This nitrogen is then converted into organic forms, such as amino acids, which serve as building blocks for proteins.

NITROGEN ASSIMILATION

1.0Introduction

Nitrogen assimilation is a biological process by which organisms assimilate nitrogen from inorganic or organic sources into organic molecules, mainly to synthesize amino acids, nucleotides, and other nitrogen-containing compounds necessary for life. This process forms the basis of the nitrogen cycle and occurs in plants, microorganisms, and animals.

Nitrogen exists in various forms in the environment, including:

  • Inorganic forms: Nitrate , nitrite and ammonium .
  • Organic forms: Amino acids and proteins obtained from food or decomposition.

2.0Steps in Nitrogen Assimilation

The process varies slightly between plants, microorganisms, and animals but generally involves these steps: In Plants and Microorganisms

  1. Nitrate Uptake: Plants and some microorganisms absorb nitrate from the soil using specialized transport proteins in their root cells.
  2. Reduction of Nitrate to Ammonium:
  • Nitrate reductase converts nitrate  to nitrite .
  • Nitrite reductase reduces nitrite to ammonium .
  1. Incorporation into Organic Compounds:
  • Ammonium (NH4+​) is incorporated into amino acids via enzymes such as glutamine synthetase and glutamate synthase. 
  • Glutamine serves as a donor of nitrogen for synthesizing other amino acids and biomolecules.

Steps in Nitrogen Assimilation

  • Animals do not fix atmospheric nitrogen or reduce nitrate; instead, they assimilate nitrogen by consuming organic nitrogen (proteins) from food. Proteins are digested into amino acids, which are absorbed and used for biosynthesis.
  • In Microorganisms, Some bacteria (e.g., nitrogen-fixing bacteria) can convert atmospheric nitrogen gas into ammonium in a process called nitrogen fixation, which precedes assimilation.

3.0Importance of Nitrogen Assimilation and involved Enzymes

Nitrogen assimilation is essential for crop growth. Farmers always use fertilizers to provide an adequate amount of nitrogen.

  • Amino Acid Synthesis: It is essential for protein synthesis.
  • Nucleotide Synthesis: It is required for DNA and RNA synthesis.
  • Chlorophyll Formation: Nitrogen is a part of chlorophyll, which is essential for photosynthesis in plants.
  • Ecosystem Function: It facilitates the flow of nitrogen through the biosphere, which connects atmospheric, terrestrial, and aquatic systems.

Importance of Nitrogen Assimilation and involved Enzymes

  • Nitrate Reductase: Catalyzes the reduction of nitrate to nitrite.
  • Nitrite Reductase: Converts nitrite to ammonium.
  • Glutamine Synthetase: Incorporates ammonium into glutamine.
  • Glutamate Synthase (GOGAT): Transfer of nitrogen from glutamine into the formation of glutamate.

Nitrogen assimilation is, therefore, the fundamental cornerstone connecting biological processes to ecological and agricultural systems.

4.0Nitrogen Cycle

Nitrogen is present as dinitrogen (N2) in the air, where the two Nitrogen are held together by triple covalent bonds. Only a few organisms like bacteria, blue-green algae (cyanobacteria) are able to utilize and fix atmospheric nitrogen. Therefore it has to be converted into other forms for use in absorption by plants and other organisms.

Nitrogen Cycle

The nitrogen cycle consists of nitrogen fixation, ammonification, nitrification, denitrification and assimilation.

  • Nitrogen fixation- It is the conversion of atmospheric nitrogen to ammonia. Nitrogen fixation can take place naturally through lightning and UV radiation. Another aspect of nitrogen fixation involves industrial processes and by the action of living organisms as well. The reduction of nitrogen to ammonia by a living organism is known as the bioloically carried out nitrogen fixation.  
  • Ammonification – Ammonification is the decomposition process of dead and dying organic matter that results in ammonia.
  • Nitrification – The process of conversion of ammonia to nitrite and nitrate in the soil by bacteria is called nitrification. Nitrite is first formed from ammonia by the bacteria Nitrosomonas and Nitrococcus and then it is further oxidised to nitrate by the bacterium Nitrobacter.
  • Denitrification – Nitrate in the soil also gets converted back to nitrogen by the process of denitrification. Bacteria like Pseudomonas and Thiobacillus carry out denitrification.
  • Assimilation- it is the process by which nitrates and ammonia become used to form organic compounds.

Table of Contents


  • 1.0Introduction
  • 2.0Steps in Nitrogen Assimilation
  • 3.0Importance of Nitrogen Assimilation and involved Enzymes
  • 4.0Nitrogen Cycle

Frequently Asked Questions

Nitrogen assimilation is the process through which living organisms convert inorganic nitrogen from sources such as ammonia or nitrate into organic compounds, primarily amino acids, which are required for protein synthesis and other essential cellular functions.

Nitrogen fixation is the conversion of atmospheric nitrogen (N2) into ammonia (NH3) or related compounds, primarily carried out by certain bacteria and archaea. This process is essential for making nitrogen available to plants, as they cannot directly use atmospheric nitrogen.

Plants absorb nitrogen in the form of nitrate (NO3−) and ammonium (NH4+), both are available in the soil, whereas atmospheric nitrogen (N2) can also assimilated by certain nitrogen fixing bacteria.

Microorganisms, including bacteria and fungi, form the basis of assimilation where they break down organic matter and convert inorganic forms of nitrogen compounds into organic forms that can be readily used by plants. Various bacteria fix atmospheric nitrogen in the form of ammonia hence increasing soil fertility.

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