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The Chemistry and Fertility of Soils under Tropical Weeds   91



                           bacteria may fix atmospheric N.  This N is eventually  available to plants after the
                           bacteria are dead and decayed.
                              The protein-N is not available to plants and, therefore, plants cannot utilize it
                           before this protein-N is converted into inorganic forms that are available to plants.
                           Various soil microorganisms decompose and detach the protein-N in the form of
                           NH 3 , which will encounter an ammonification process upon reaction with water to
                                  +
                                                                                        +
                           form NH 4 .  Ammonium is easily absorbed by plant roots.  However, NH 4  usually
                           cannot suffice the plant need of N except for paddy plants.
                              Ammonium ions are then oxydized by particular bacteria through a two step
                                                                                 +
                                                                                         -
                           reactions  called  nitrification.    This  reactions  change  of  NH 4   to  NO 2   with
                                                                   -      -
                           Nitrosomonas as the oxydizing agent and of NO 2  to NO 3  with Nitrobacter as the
                           oxydizing agent (Bartlett, 1981).  These reactions follow Eq. 6.2 and Eq. 6.3.

                                  +              -     +
                              2 NH 4   +  3 O 2       2 NO 2   +  4 H   +  2 H 2 O   .......   Eq. 6.2

                                               -
                                  -
                              2 NO 2   +  O 2      2 NO 3    .......   Eq. 6.3

                           The above reactions can be summarized as shown by Eq. 6.4 as follows.

                                  +             -    +
                              2 NH 4   +  2 O 2       NO 3   +  2 H   +  H 2 O   .......   Eq. 6.4
                           This reaction shows that the nitrification process needs the presence of enough O 2 .
                           The nitrification does not occur in waterlogged  soils because the absence of O 2 .
                           This reaction also suggests that the soil porosity controls the nitrification process.
                           Eq.6.4 also shows that the nitrification acidify soils as indicated by the production
                              +
                           of H  ions.
                              Wu et al. (2011) report that the Ammonia Oxidizing Bacteria sharply increased
                           about 50 times in soils fertilized with long-term N.  This indicates that nitrification
                           process occurs faster in the presence of N fertilizers.  For example, the presence of
                                                                          +
                           Urea  increases  NH 3   which  very  quickly  becomes  NH 4   upon  hydrolysis.    The
                           decomposition of urea that produces NH 3  progresses as shown in Eq. 6.5 as follows
                           (Tabatabai,1982).

                              NH 2 CONH 2  + H 2 O    CO 2  + 2 NH 3    .......   Eq. 6.5

                                                          +
                           The production of NH 3  and, hence NH 4 , is higher in the presence of enough water
                           and is accelerated by the presence of enzyme  Urease, the activity of which  was
                           reported  to  increase  with  the  increase  in  applied  Urea-N  (Kumar  and  Wagenet,
                                                          Abdul Kadir Salam and Nanik Sriyani  – 2019
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