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The Chemistry and Fertility of Soils under Tropical Weeds   21



                           previously, these changes may affect the soil pH, which is very closely related to
                           the soil mineral matter weathering through dissolution processes.  The dissolution
                           processes are more vigorous at low pH (Salam, 1989).  The changes in soil pH not
                           only affect the soil mineral weathering, but as pointed out previously, also affect
                           several other soil chemical properties such as soil CEC and BS (Salam, 2017; Salam,
                           2019).
                              Like soil mineral matters, soil organic matters are most likely affected by the
                           presence of weeds since weeds may also produce soil enzymes like phosphatases,
                           aryl-sulfatases, proteases, etc.  In the presence of soil enzymes, the decomposition
                           of soil organic matter is speeded.  The mineral matter weathering and the organic
                           matter  decomposition  may  produce  nutrient  elements  and  substances  that  may
                           change  the  chemical  properties  of  the  soil  system.    These  two  processes  that
                           release nutrient elements and other substances into the soil water may complete
                           the relationship between soil – nutrient element – water – weeds as a system.



                           2.1  The Soil – Water – Nutrient – Weed Relationships

                              The  relationship  between  soil,  water  (soil  water),  nutrient  elements,  and
                           weeds is depicted in Fig. 2.1.  Weed roots are directly connected to the soil water
                           where  they  absorb  most  of  the  nutrient  elements  needed  for  their  growth  and
                           development.   As they are competitive and progressive,  weeds  may significantly
                           absorb the  soluble nutrient  elements from  soil water.    Of course, absorption by
                           weeds  is  not  the  only  mechanism  for  nutrient  element  losses  in  the  soil
                           environment.    The  soluble  nutrient  elements  in  soil  water  are  also  absorbed  by
                           plants and parts of it may be adsorbed by the soil adsorption sites, precipitated, or
                           leached.  However, the presence of weeds may lower the nutrient element losses
                           through  all  these  mechanisms  and  increase  that  lost  by  weeds.  Therefore,  this
                           stimulates farmers to eradicate weeds employing several mechanisms.
                              The above explanation shows that weeds may cause a significant effect on the
                           nutrient  element  balance  in  the  soil  environment.    The  imbalance  of  nutrient
                           element  in  soil  water  is  chemically  buffered  by  some  mechanisms  mentioned
                           previously.  The first mechanism is the detachment of adsorbed nutrient elements
                           as described in Eq. 2.1 called desorption.

                              X – NE      X –    +   NE   …….   Eq. 2.1

                                                          Abdul Kadir Salam and Nanik Sriyani  – 2019
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