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The Chemistry and Fertility of Soils under Tropical Weeds   29



                           element concentrations but also by the changes in other soil properties like soil pH
                           and  soil  E.    The  decrease  in  soil  pH  is  shown  to  stimulate  not  only  the  nutrient
                           release  through  cation  exchange  but  also  through  dissolution  of  soil  secondary
                           minerals.

                                                   -
                                           2+
                              Fe(OH) 2      Fe   +  2 OH    …….   Eq. 2.10

                                         -]2
                                    2+
                              K  =   [Fe ] [OH    …….   Eq. 2.11

                              The  decrease  in  soil  E  may  reduce  the  related  nutrient  element  in  soil
                           secondary minerals like Fe 2 (HPO 4 ) 3  and release the nutrient element cations into
                           the soil solution.  The trivalent Fe cation ion the structure of Fe 2 (HPO 4 ) 3  is released
                                                           2+
                               2+
                           as Fe  ion in soil water.  Therefore, Fe  is more readily available in flooded soils
                                               3+
                           like paddy soils, while Fe  in dry soils is not available because its association among
                           which with P.

                                                     2+
                                                              2-
                              Fe 2 (HPO 4 ) 3   +   2 e -       2 Fe    +   3 HPO 4    …….   Eq. 2.12

                           On  the  other  hand,  S  is  not  available  in  flooded  soil  because  it  presents  as  FeS
                           precipitates.    The  S  may  be  oxidized  upon  the  increase  in  soil  E  by  draining  the
                                                                                      2-
                                                                              3+
                           flooded soils following Eq. 2.13.  FeS may dissolve producing Fe  and SO 4 .

                                                            +
                                                     2-
                                              3+
                                                                  -
                              FeS  + 4 H 2 O    Fe    +   SO 4   +   8 H    +   9 e     …….   Eq. 2.13

                              In  addition  to  soil  secondary  minerals  (precipitates),  there  are  also  primary
                           minerals  containing  various  kinds  and  amounts  of  nutrient  elements.    Some
                           primary minerals  present in  the soil environment  and their chemical weathering
                           are listed in Table 2.4.  The primary minerals may release their structural nutrient
                           elements  through  the  process  of  weathering  (Table  2.2  and  Table  2.3).    One
                           example of the weathering process is the release of structural K from K-feldspar
                           (Orthoclase, KAlSi 3 O 8 ) as shown in Eq. 2.14.

                                                    +
                                                        3+
                                              +
                              KAlSi 3 O 8  + 4 H 2 O + 4 H       K  + Al  + 3 Si(OH) 4    .......   Eq. 2.14

                                +
                           Free K  is released into the soil water increasing the soil water K concentrations.
                           This reaction is a non-equilibrium reaction and so it will progress and speed up in
                                                  +
                           the presence of water and H  ions.
                                                          Abdul Kadir Salam and Nanik Sriyani  – 2019
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