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32   The Chemistry and Fertility of Soils under Tropical Weeds



                           temperature, and C/N ratios give an indirect effect of the enhancement of organic
                           matter  decomposition.    As  stated  in  Salam  (2014),  soil  water,  soil  N,  and  soil
                           temperature  influence  the  growth  of  soil  enzyme  producing  microorganisms.    In
                           general the soil microbial population and activity, and thereby the activities of soil
                           enzymes,  increase  with  the  increase  in  water  content,  N  content,  and  soil
                           temperature. In particular for phosphatases, their activities below the optimum pH
                           increase with the increase in soil pH.  Optimum pH is the value of pH at which the
                           activity of phosphatases is maximum.


                           2.3  The Effects of Weeds on Nutrient Element Release

                                from Soil Minerals and Organic Matters

                              Chemicals  released by weed roots may directly and indirectly affect the soil
                           properties that might intensify the releases on nutrient elements from soil solids.
                           The  depletion  in  soil  pH  in  the  root  zones  of  weeds  may  directly  increase  the
                           process of soil mineral weathering releasing nutrient elements into the soil water.
                           Salam et al. (2019) report that several weeds stimulate the release of K from soil
                           minerals.  The effectiveness of weed plants in stimulating the release of soil K were:
                           A. Pintoi > A. gangetica > Widelia sp. > P. conjugatum > P. purpureum.  A. pintoi is
                           suggested to be the most effective in stimulating the release of K from soil minerals
                           as  proven  by  the  positive  values  of  Exch.  K  [  Exch.  K  =  Final  Exch.  K  (After
                           Planting)    –  Initial  Exch.  K  (Before  Planting).  This  phenomenon  is  related  to  its
                           higher Root-To-Shoot Ratio compared to others.
                              The increase in soil water cations is not only attributed to the weathering of
                           soil minerals but also to the decomposition of soil organic matter directly speeded
                           by  various  soil  enzymes  excreted  by  weed  roots  and  their  associated
                           microorganisms. Therefore, the increase in soil exchangeable K in the root-zones of
                           A.  pintoi  reported  by  Salam  et  al.  (2019)  might  have  also  been  related  to  this
                           phenomenon.
                              Combined with decrease in soil CEC in response to the decrease in soil pH, the
                           increase in nutrient element concentration in soil water may indirectly cause the
                           increase  in  soil  exchangeable  cations.  However,  the  presence  of  weed-roots
                           absorbing cations may cause the real exchangeable cations in soils to decease.  This
                           phenomenon is reported by Salam et al. (2019), the soil exchangeable K was lower
                           in  the  presence  of  weeds  like  A.  gangetica,  Widelia  sp.,  P.  conjugatum,  and  P.
                           purpureum.  A. pintoi is different, demonstrating its effectiveness in stimulating the

                           Abdul Kadir Salam and Nanik Sriyani – 2019
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