Page 125 - Ilmu Tanah Book
P. 125

112   The Chemistry and Fertility of Soils under Tropical Weeds















                           Chapter 7


                           Effects of Tropical Weeds on Soil

                           Potassium




                                                          7.1  The Release of Potassium from Soil Minerals
                                                    7.2  The Release of Potassium from Soil Organic Matters
                                                       7.3  The Effects of Soil pH on Soil Potassium Release
                                                        7.4  The Effects of Weeds on Soil Potassium Release
                                                                                    Key Questions



                           A
                                 s  previously  stated,  the  weed  root  excretion  may  lower  the  soil  pH  and
                                 increase the soil enzymatic activities.  These chemical changes may bring
                                 about the changes in other soil chemical and fertility properties.  Among
                           the most important change is the increase in dissolved and exchangeable K of soils.
                           Of course with a prerequisite that the related soils contain adequate organic and
                           inorganic sources of K easily transformed into readily available form for plants by
                           chemical weathering and enzymatic decomposition.
                                                 +
                              The accumulation of H  ions may cause the soil K-mineral dissolution.  In the
                                      +
                           presence  of  H   and  water,  orthoclase,  which  is  one  of  the  K  sources  of  silicate
                           minerals may detach its structural K increasing the dissolved K in the soil solution
                           and in turn may enhance the soil exchangeable K.  Any other sources of K may also
                           dissolve  increasing  these  available  forms  of  K  in  the  soil  environment.    Some

                           Abdul Kadir Salam and Nanik Sriyani – 2019
   120   121   122   123   124   125   126   127   128   129   130