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The Chemistry and Fertility of Soils under Tropical Weeds   87



                           and  organic  matter  (organic  matter  is  about  1.7  times  of  organic  C),  as  well  as
                           organic N, organic P, and organic S.
                              Organic  C,  N,  P,  and  S  are  released  into  the  soil  environment  by  two
                           mechanisms,  through  direct  and  indirect  mechanisms.    First,  organic  C  is
                           continuously released through weed rooting system as organic acids.  In addition to
                           acidify the ambient soils, the release of organic acids may surely increase the soil
                           organic C.  Second, organic C, N, P, and S can be enhanced indirectly through the
                           decomposition of dead weed parts like dead roots and shoots.  The hydrocarbon
                           composed by weeds through photosynthesis may encounter a reverse reaction so-
                           called decomposition that may produce more stable organic matters containing C
                                                                   -
                           and CO 2  that may react with water forming HCO 3  and also inorganic N, P, and S. All
                                                                            -    2-       2-
                           organic matters may finally decompose producing CO 2 , NO 3 , HPO 4 , and SO 4  and
                           complete the nutrient-cycles.  Competitive and progressive weeds may contribute
                           significantly to the increase in soil organic C and organic matter and probably to the
                           soil nutrients..



                           6.1  Nutrient Cycles

                              The influence of weeds on soil C, N, P, and S is closely related to the cycles of
                           these nutrient elements in the soil environment (Fig. 6.1, Fig. 1.7, Fig. 1.8, and Fig.
                           1.9).  The so-called C-cycle is the transformation of organic matters to their more
                           simple constituents that are available for plant root absorption continued by the
                           absorption  of  these  constituents  by  plant  roots  and  the  following  formation  of
                           organic substances through photosynthesis in the plant-leaf chlorophylls (Fig. 6.1).
                           The  destruction  of  organic  matters  into  their  constituents  that  are  available  to
                           plant  involved  microorganisms  called  decomposers.    Decomposers  are  of  great
                           importance  in  the  C-Cycle  that  also  involve  Producers  (plants  with  chlorophylls),
                           Consumers (animals and humans), and Decomposers (microorganisms).  Without
                           Decomposers,  organic  matters  contributed  by  vegetation  like  weeds  may
                           accumulate in the environment causing various problems because the cycle is not
                           completed.
                              Soil microorganisms are small in size and are present in soils in great numbers.
                           The  general  rule  is  that  the  smaller  the  sizes  of  the  microorganisms  the  greater
                           their numbers (Singer and Munns, 1987).  The smaller size also causes the more
                           significant  role  in  the  environment.    One  gram  of  soil  may  contain  around  one
                                                          Abdul Kadir Salam and Nanik Sriyani  – 2019
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