3. INTRODUCTION
The nitrogen cycle is the process by which nitrogen is
converted between its various chemical forms. This
transformation can be carried out via both biological
and non-biological processes. Important processes in
the nitrogen cycle include fixation, mineralization,
nitrification, and denitrification. The majority of
Earth's atmosphere (approximately 78%) is nitrogen.
6. NITRIFICATION
The atmospheric nitrogen is fixed by nitrogen fixing
bacteria to yield ammonia. This ammonia is used by
living microorganism and converted into nitrate.
NH4+ = NO2- ( Nitrosomonas)
NO2-
= NO3- ( Nitrobactor)
7. Denitrification
The conversion of nitrate to nitrogen under anaerobic
condition is known as denitrification.
NO3- = N2 (Bacillus, Prococus, pseudomonas)
8. ANAMMOX
In this biological process, nitrite and ammonium are
converted directly into dinitrogen gas. This process
contributes up to 50% of the dinitrogen gas produced
in the oceans. It is thus a major sink for fixed nitrogen
and so limits oceanic primary productivity. The
overall catabolic reaction is:
NH4+ + NO2− → N2 + 2H2O. (Brocadia)
The bacteria that perform the anammox process
belong to the bacterial phylum planctomycetes of
which Planctomyces and Pirellula are the best known
genera.
9. AMMONIFICATION
Ammonia Is released during the decomposition of organic
nitrogen compound such as amino acids and nucleotides a
process called ammonification.
Organic N2 =NH4+
( Rhizobium)
16. Nif Genes
The nif gene is the gene responsible for the coding of
proteins related and associated with the fixation of
atmospheric nitrogen into a form of nitrogen
available to plants. These genes are found in nitrogen
fixing bacteria and cyanobacteria.