Page 19 - Enzymes in Tropical Soils
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Enzymes in Tropical Soils   7


                           and adsorption by soil particle surfaces.  This releasing process (Decomplexation) is
                           determined  by  an  equilibrium  constant  (K)  for  complexation.    The  higher  the  K
                           value the more difficult for the main cation to be released.  Some common free
                           ions and their complex ions in the soil water system are listed in Table 1.2.


                                    Table 1.1.  Several mechanisms releasing free ions along with their
                                                controlling factors (Salam, 2012).

                               No.    Mechanisms        Sources         Dominant Controlling
                                                                             Factors
                                1   Decomplexation   Complex Ions    K*
                                2   Dissolution     Precipitates     Ksp*
                                3   Desorption      Exchangeable Ions   K*, CEC, pH, Preference,
                                4   Weathering      Soil Mineral     pH, Soil Water, and Mineral
                                                    Structures       Structure, Composition, and
                                                                     Chemistry
                                5   Decomposition   Soil Organic     pH, Soil Water, Enzymatic
                                                    Structures       Activities, Temperature, C/N
                                                                     Ratios, Microbial Populations
                                                                     and Activities

                             *K  is  an  equilibrium  constant  related  to  a  particular  chemical  reaction;  K sp   is  an
                             equilibrium constant related to dissolution of a precipitate.

                                The major cations and the minor cations show different behaviors towards
                           complexation processes.  The differences are subjected to the affinities of elements
                           towards ligands.  The concentrations of free ions and their related complex ions of
                           some elements are listed in Table 1.3.  It is obvious that the free ions of the major
                                        2+
                                             +
                                                   +
                                   2+
                           cations Ca , Mg , Na , and K  are about 70 – 90% of their respective total soluble
                                                                             2+
                           concentrations in soil solution.  The concentration of free Zn  is about 40% of the
                           total soluble Zn.  Copper shows a very high  affinity towards ligand; only 2% of the
                                                                 2+
                           total  soluble  Cu  is  in  the  form  of  free  Cu   (Ellis  and  Knezek,  1982).    This
                                                    2+                                    2+
                           phenomenon indicates that Cu  is more strongly complexed compared to Zn  and
                           also compared to the soil major cations.
                                In addition to those in the forms of complex ions, part of nutrient elements
                           are  present  in  the  forms  of  precipitates.    The  dissolution  of  precipitates  is
                           controlled  by  their  equilibrium  constants  (K sp )  and  solubility  products,  which  are
                           the product of all product species concentrations.  For example:



                                                                          Abdul Kadir Salam - 2014
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