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140   The Chemistry and Fertility of Soils under Tropical Weeds



                           root  absorption  or  leaching,  the  heavy  metals  in  complexes,  chelates,  adsorbed
                           sites,  or  precipitates  will  be  released  to  compensate  the  respective  equilibrium
                           constants through equilibrium processes.  On the other hand, if the concentrations
                           of free ionic heavy metals in soil water are high enough due to external addition
                           such as waste and fertilizer applications, parts of the free ionic heavy metals in soil
                           solution will be complexed, chelated, adsorbed, or precipitated, depending on the
                           pertaining conditions to reach new equilibrium values.




                                                        Wastes
                                  Organics                                    Plants
                                                         Fertilizers
                                    Minerals
                                                           Pesticides
                                      Adsorbed


                                     Complexes             Free Ions           Chelates


                                                                Leaching
                                     Precipitates




                              Fig. 8.1.  The relationships between forms of heavy metals in the soil environment
                                            (Adapted from Salam, 1997a; Salam, 2017).



                                                                               2+
                              Cavallaro and McBride (1980) reports that the free ionic Cu  concentration in
                           the soil system was greatly pH-dependent, but the concentration was below the
                           levels  needed  for  the  precipitation  processes  to  occur.  Abd-elfattah  and  Wada
                                                 2+  2+  2+   2+      2+                -7    -
                           (1981) also suggest that Zn , Pb , Cu , Co , and Cd  at concentrations 10  to 10
                           2      -3    -2
                            M in 10  to 10  M CaCl 2  were not precipitated as hydroxides but were adsorbed
                           by cation-exchange sites.  Salam and Helmke (1998) also report that the logarithmic
                               2+
                           of  Cu   concentration  was  linearly  related  to  the  soil  pH  and  was  controlled  by
                           adsorption-desorption  process  (Fig.  8.2).    The  importance  of  each  chemical

                           Abdul Kadir Salam and Nanik Sriyani – 2019
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