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Agriculture for Secondary Schools


          Table 2.1: Translation of soil pH
                Soil reaction             pH range                  Description

          Acidic                           3.5 - 4.0        Extremely acid
                                           4.1 - 5.0        Strongly acid
                                           5.1 - 6.0        Moderately acid
                                           6.1 - 6.9        Slightly acid
          Neutral                             7.0           Neutral
          Alkaline                         7.1 - 8.0        Slightly alkaline
                                           8.1 - 9.0        Moderately alkaline
                                           9.1 - 10.0       Strongly alkaline
                                          10.1 - 11.0       Extremely alkaline

          Sources of hydrogen ions in soil and causes of soil acidity

          Hydrogen ions in soil originate from various sources. There are three major and
          other minor sources of hydrogen ions in soil solution. These include:
          (a)  Carbonic acid produced after carbon dioxide dissoved in soil water: Carbonic
              acid produced when carbon dioxide (CO ) from decomposing organic matter,
                                                      2
              root respiration, and the soil atmosphere is dissolved in the soil water as it is
              shown in the following equation:
                                      CO  + H O ! ⇀!!  H CO
                                                  ↽ !!!
                                         2    2         2   3
              When H CO  dissociates, it yields hydrogen ions as it is shown in the following
                      2
                          3
              equation:
                                      H CO  ! ⇀!!   H  + HCO  -
                                                    +
                                       2   3  ↽ !!!          3
          (b)  The  aluminium  ions  that  are  adsorbed on  the  soil  colloidal  particles:  This
              refers to the reaction of aluminum ions (Al ) with water. When the soil pH is
                                                        3+
              extremely low, aluminium becomes very soluble. Under such condition, a lot
              of aluminium ions are adsorbed on soil colloids. The adsorbed aluminium is in
              equilibrium with Al  ions which are present in the soil solution. Aluminium
                                 3+
              ions present in soil solution release hydrogen ions after hydrolysis, that is, after
              reacting with water. The hydrogen ions released are thus added to soil solution
              as it is shown in the following equation:
                        3H O     +     Al 3+              Al(OH) 3          +       3H +
                           2
                        Water   Aluminium      Aluminium        Hydrogen
                                           ions     hydroxide     ions

          (c)  The hydrogen ions that are adsorbed on the soil colloidal particles: The amount
              of any element that is adsorbed on the colloids is normally in equilibrium with
              the amount of that particular element which is present in the soil solution. When

                                                                    Student’s Book Form Three
            36




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   AGRICULTURE FORM 3   9.11.2022.indd   36                                               10/01/2025   12:31
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