Page 210 - Enzymes in Tropical Soils
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198     Enzymes In Tropical Soils



















                           GLOSSARY



                           Acidification is to make a reaction medium to have a lower pH.  For example, soil
                                acidification is to make the soil pH lower by using S powder or naturally by
                                root excretion of organic acids or by producing CO 2  during root respiration.

                           Activation  Energy  is  a  measure  on  the  magnitude  of  all  forces  that  must  be
                                surmounted during a reaction process (Sparks, 1989).  This energy barrier
                                separates the reactant state from the product state (Castellan, 1983).  To
                                form the products, the reactants must have sufficient energy to overcome
                                this energy barrier.  Without enough energy to surmount the energy barrier,
                                the reactants will stay at their origiinal states and the products will never
                                exist.
                           Adsorption is a chemical process by which an ion is attached to a solid  with an
                                opposite charge.  For example, the adsorption of  a cation by the negative
                                charges of soil organic matters.
                           Alkalination  is  to  make  a  medium  to  have  a  higher  pH.    For  example,  soil
                                alkalination is to make the soil pH higher by a liming materials such as calcite
                                or dolomite.  In general it is referred to as liming.
                           Arylsulfatase is an organic substance produced by microorganisms, earthworms, or
                                plant roots acting as a biocatalyst functioning to accelerate the detachment
                                                                       2-
                                of  S  from  organic  S  to  form  inorganic  SO 4   available  for  plant  root
                                absorption.



                           Abdul Kadir Salam - 2014
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