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The Chemistry and Fertility of Soils under Tropical Weeds   115



                           Table  7.2.  Potassium  adsorbed  on  soil  solids  called  exchangeable  K  is  released
                           through  desorption  process  and  controlled  by  equilibrium  constant  (K),  cation
                           exchange  capacity  (CEC),  soil  pH,  and  solid  preference  towards  cations.
                           Exchangeable  K  is  released  when  its  concentration  in  soil  solution  is  lowered  by
                           some  mechanisms  like  plant  root  absorption  and  leaching.    The  release  is  more
                           difficult when the soil CEC and pH are high and the soil preference towards K is
                           high.  Therefore, the release of the exchangeable K is easily enhanced by lowering
                           the soil pH, increasing the concentration of competing cations, and lowering the
                                                    +
                           soil solution concentration of K .


                              Table 7.2.  The mechanisms of plant nutrient release and their controlling factors.


                                                                              Dominant
                                        Chemical
                                No.                    Sources of Free Ions   Controlling Factors
                                        Processes
                                 1   Decomplexation    Complex Ions       K*

                                 2   Dissolution     Precipitates         K sp *

                                 3   Desorption      Exchangeable K       K*, CEC, pH,
                                                                          Preference


                                 4   Weathering      Mineral Structural K   pH, Soil Moisture,
                                                                          Mineral Structure,
                                                                          Mineral Chemical
                                                                          Composition


                                 5   Decomposition   Organic Structural K   pH, Soil Moisture,
                                                                          Enzymatic Activity,
                                                                          Temperature,  C/N
                                                                          Ratio

                               *K is an equilibrium constant related to the related chemical reaction, K sp  is an
                               equilibrium constant related to the dissolution of a precipitate


                                                          Abdul Kadir Salam and Nanik Sriyani  – 2019
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