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14   The Chemistry and Fertility of Soils under Tropical Weeds



                           grow  more  extensively  and  competitively.    They  produce  more  biomass  and
                                         +
                           probably more H  ions, organic acids, and CO 2  that acidify the soil environment.
                           Their acidifying effect may be greater in soils planted with weeds with high root-to-
                           shoot ratios. High root-to-shoot ratios and production of acidifying substances may
                           cause  high  capability  of  weeds  to  dissolve  soil  minerals  containing  nutrient
                           elements such as K, Ca, Mg, and micronutrients.
                              Arachis pintoi showed higher root-to-shoot ratio than did Asystacia gangetica,
                           Widelia sp., Paspalum conjugatum, and Pennisetum purpureum (Ontia, 2018; Salam
                           et al., 2019).  A. pintoi showed the highest effectiveness in stimulating the release
                           of K from infertile soil of Ultisol Tanjung Bintang from South Lampung and from
                           fertile soil of Mollisol Jabung from East Lampung.  Their effectiveness follows the
                           sequence of A. pintoi > A. gangetica > Widelia sp. > P. conjugatum > P. purpureum.
                           The released K was reported to be well-correlated with the dry-weight of root and
                           shoot.
                              The conceptual mechanisms of weed roots in affecting the soil properties are
                           described in Fig. 1.10.  As pointed out previously, the weed roots may release the
                            +                                              +   2+   2+  2+   2+
                           H  ions in exchange of the absorption of cations including K , Ca , Mg , Cu , Zn ,
                           etc.    The  root  respiration  may  also  release  CO 2   that  upon  reaction  with  water
                                            +
                           molecules produces H  ion as shown by Eq. 1.5.

                                              +      -
                              CO 2    +   H 2 O     H   + HCO 3    …….   Eq. 1.5


                                                                           +
                              These processes may increase the concentration of H  ions, which may then
                           attack the nutrient element position in the structure of soil minerals.  As reported,
                                       +
                           the  released  K   and  other  nutrient  elements  are  intensified  by  the  presence  of
                                 +
                           more  H   ions  (Johnston  and  Olsen,  1972;  Manley  and  Evals,  1986;  Salam,  1989;
                           Najafi-Ghiri and Jabari, 2013).  The excreted organic acids by weed roots may also
                           lower  the  ambient  soil  pH  and  intensify  the  effectiveness  of  weed  roots  in
                           stimulating the release of nutrient elements from soil minerals matters.
                              The  production  of  various  enzymes  by  weed  roots  and  microorganisms
                           stimulated  by  the  presence  of  weed  roots,  such  as  phosphatases,  arylsulfatase,
                           proteases, etc., may accelerate the decomposition of soil organic matters releasing
                           various  nutrient  elements  from  the  organic  matter  structures.    This  process  of
                           decomposition along with the weathering of soil mineral matters may accumulate
                                     +
                           the soluble K  and other nutrient elements in the soil solution.




                           Abdul Kadir Salam and Nanik Sriyani – 2019
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