Page 156 - Enzymes in Tropical Soils
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144     Enzymes In Tropical Soils


                           (Helling et al., 1964; Tan and Dowling, 1984; McGrath et al., 1988; Alloway 1990b;
                           Parfitt et al., 1995; Rodella et al., 1995; Bang and Hesterberg, 2004; Brown et al.,
                           2004; Stuczynski et al., 2007; Buss et al., 2012; Smolders et al., 2012).  It was also
                           reported by Saidy and Badruzsaufari (2009) that the increase in soil organic matter
                           contents decreases the soil Cr (VI) concentration.  The functional groups or organic
                           matters in soils might have dehydrogenized and arised negative charges that then
                           complexed or adsorbed free ionic heavy metals particularly at alkaline pH.  Rodella
                           et  al.  (1995)  reported  that  the  CEC  of  Horizon  A  and  Horizon  B  in  some  New
                           Zealand soils were originated from the soil organic matter carboxylic groups.  The
                           maximum capacity of heavy metals can be adsorbed by soil organic matters was
                           equivalent to the amount of the soil carboxylics groups (Alloway, 1990b).


                                         Table 9.8.  The relationship between Cd, Cu, and Zn
                                                    solubilities with soil pH.

                                        No    Heavy Metal   Equation

                                                                2+
                                        1         Cd       Log (Cd ) = 6.50 – 2 pH
                                                                2+
                                        2         Cu       Log (Cu ) = 2.80 – 2 pH
                                                                2+
                                        3         Zn       Log (Zn ) = 5.80 – 2 pH
                                      Taken from Lindsay (1979), Workman and Lindsay (1990), Ma
                                      and Lindsay (1990), El-Falaky et al. (1991)

                                Organic matter contributes about 32% of the soil CEC (Rodella et al., 1995).
                           If  the  soil  pH  is  also  considered,  the  contribution  of  organic  matters  to  soil  CEC
                           increases to be 78%, indicating that soil pH is a very important factor to consider to
                           immobilize heavy metals in soils.  The importance of pH is not only related to the
                           non-specific  adsorption  of  heavy  metals,  but  also  to  the  specific  adsorption
                           involving the formation of covalent bonding.  However, the specific adsorption of
                           heavy  metals  is  more  important  because  the  soil  capacity  related  to  this
                           mechanisms is higher than do the non-specific adsorption.  The decrease in heavy
                           metal solubility as affected by lime (that increase the soil pH) and organic matter
                           (that increase the soil adsorptive capacity) is shown in Fig. 9.11.
                                Fig.  9.11 clearly shows that heavy metals of industrial wastes available to
                           plant root absorption are lowered because part of the heavy metals are adsorbed
                           by soil clay and organic matter colloids with increased adsorption capacities as a
                           result of lime and/or organic matter treatments.  This phenomenon is more clearly



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