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76   The Chemistry and Fertility of Soils under Tropical Weeds



                           Amaranth (Amaranthus tricolor L.).  The pH in the root zones of these vegetation
                           were 6.25, 5.03, 5.01, and 5.64, respectively.
                              One  good  example  of  anthropogenic  acidification  is  related  to  the  intensive
                           use of Urea in agriculture.  Urea is an important commercial source of N commonly
                           used, particularly in Indonesia.  Since it contains one of the major plant nutrients,
                           the use of Urea is huge, and in greater amount than those of other major nutrients
                           such  as  P  and  K.    However,  the  use  of  Urea  may  cause  acidification  as  seen
                           chemically in Eq. 5.2 as follows:

                              NH 2 CONH 2  + H 2 O    CO 2  + 2 NH 3    .......   Eq. 5.2.


                           The  Urea  molecule  is  hydrolyzed  to  produce  carbondioxide  and  ammonia
                           molecules.  The carbondioxide molecules may then react with water molecules to
                                   +
                           produce H  ion as indicated by Eq. 5.1.  Ammonia molecules after being protonated
                                                                                +
                           to be an ammonium ion will encounter nitrification to produce H  ions (Eq. 5.3) as
                           follows:

                                  +             -    +
                              2 NH 4   +  2 O 2       NO 3   +  2 H   +  H 2 O   .......   Eq. 5.3.

                           The above two processes (Eq. 5.2 and Eq. 5.3) may eventually decrease the soil pH.
                           A long term effect of the use of Urea on soil pH is shown in Table 5.2.  The soil pH is
                           shown  to  decrease  with  the  increase  in  the  amounts  of  Urea  treatments.    For
                                                                         -1
                           example, the long-term use of Urea at 200 kg Urea N ha  lowered the soil pH from
                           5.09 to 4.66, about 0.43 units.  Greater decrease occurs when the Urea treatment
                           is done in the field with intensive soil tillage.
                              According  to  Boulman  et  al.  (1995),  the  decrease  in  soil  pH  with  Urea
                                                                               +
                           treatment is attributed to two reasons: (a) the production of H  ions due to Urea
                           hydrolysis and (b) the decrease in exchangeable Ca and Mg due to replacement by
                              +
                           NH 4 .    The  decrease  in  soil  pH  due  to  long-term  application  of  Urea  has  been
                           reported  to  increase  the  soil  exchangeable  Al  and  Al  saturation  and  also  to
                                                                                          3+
                           decrease the exchangeable Ca and Mg (Schroder et al., 2011).  Because Al  is a
                           potential  source  of  acidity,  this  condition  will  worsen  the  soil  pH.    However,
                           Boulman et al. (1995) report that the decrease in pH by Urea treatment was lower
                           than that by the use of ammonia (NH 3 ).
                              Soil  acidification  may  also  happen  intentionally  in  response  to  the  need  of
                           agriculture management.  For example, soils in the pineapple plantations owned by
                           PT  Great  Giant  Pineapple  in  Central  Lampung,  Indonesia,  are  acidified  by  using



                           Abdul Kadir Salam and Nanik Sriyani – 2019
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