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40     Enzymes In Tropical Soils


                           and the rest is adsorbed on soil solids.  The soluble enzyme is the active part that
                           participates  in  the  transformation  of  organic  nutrient  elements  to  become
                           inorganic nutrient elements.
                                Geiger et al. (1998a) state that most extracellular enzymes are adsorbed on
                           organic  and  mineral  constituents.    Gianfreda  et  al.  (1992)  reported  that  the
                           equilibrium  adsorption  of  urease  on  clay  minerals  fitted  the  Langmuir  and
                           Freundlich equations.  Huang et al. (2005) reported that in the presence of organic
                           component, more enzyme molecules were adsorbed on soil clays which were more
                           easily released.  The activity of enzymes bound on soil clays was inhibited by the
                           presence of organic matter.  Coarse clays (0.2–2 mm) and inorganic soil clays had
                           higher  affinities  for  enzyme  molecules  than  fine  clays  and  organic  clays,
                           respectively.  Dharmakeerti and Thebadu (1996) states that urease is remarkably
                           stable in organo-mineral complexes found in soils.




                                       L-H

                                    Soil Depth (cm)   15-30                 Jordan River
                                       0-5
                                      .5-15





                                     30-60                                  Shawnigan Lake

                                           0      1000     2000    3000
                                                     Activity
                                                              -1
                                                                 -1
                                              (mg p-Nitrophenol g  h )


                                  Fig. 4.4.  The depth dependence of soil phosphomonoesterase activity
                                             (Redrawn from Pang and Kolenko, 1986).


                                Sarkar et al. (1989) reported that various enzymes including glucose oxidase,
                           -glucosidase,  acid  phosphatase,  tyrosinase,  and  laccases  were  immobillized  on
                           clays  and  soils  and  retained  a  large  amount  of  their  original  activities  after



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