Page 56 - Enzymes in Tropical Soils
P. 56

44     Enzymes In Tropical Soils


                           from soils.  Therefore, the presence of phosphatase in soils is very important to
                           utilyze these accumulated nutrients.  The released P in soils will then eventually re-
                           absorbed  by  plant  roots  and  re-ultilyzed  to  produce  new  organic  matters.    The
                           chain of transformation from Organic P to inorganic P by decomposition process
                           and  absorption  of  inorganic  P  through  its  re-synthesis  in  plants  to  produce  new
                           organic  matters  and  back  to  the  decomposition  of  organic  matters  to  produce
                           inorganic P is called Phosphorus Cycle or P-Cycle.  The P-Cycle is shown in Fig. 4.6.


                                                               -
                                                           H 2 PO 4
                                                              2-
                                                           HPO 4
                                                           NUTRIENTS
                                          SOIL MICROORGANISMS           PLANTS
                                           (DECOMPOSERS)              (PRODUCERS)


                                                  PHOSPHATASE


                                                                        ANIMALS
                                            ORGANIC P
                                                                      (CONSUMER I)

                                                          ANIMALS
                                                         (CONSUMER II)


                                           Fig. 4.6. The cycle of P in the soil – plant system.


                                Fig.  4.6  clearly  shows  that  the  presence  of  phosphatase  is  of  utmost
                           importance related to P in soils, since the rate of  P release is determined by its
                                                                                     2-
                           presence.  The results of its role are alcohol and orthophosphates (HPO 4 ). The role
                           of  phosphatase  is  shown  in  Eq.  4.1  as  follows  (Tabatabai,  1982).    The  action  of
                           phosphatase  on  the  organic  P  molecules  must,  however,  be  in  the  presence  of
                           enough  water  molecule.    Therefore,  the  decomposition  of  organic  P  will  be
                           inhibited  in  dry  soils.  Water  must  be  added  to  allow  the  accelerated  rates  of
                           organic P decays catalyzed by phosphatase occur in soils.

                                       2-
                                                            2-
                                RO—PO 3  + H 2 O    R—OH + HO-PO 3 .......   Eq. 4.1


                           Abdul Kadir Salam - 2014
   51   52   53   54   55   56   57   58   59   60   61