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Agriculture for Secondary Schools


          Management of soil acidity and alkalinity

          The ideal soil pH for growth of most plants as well as biological and chemical
          reactions  is between 6.5 to 7.5 Any deviation  from these pH ranges should be
          managed. The management can be either by raising the pH values or lowering it.
          pH values are raised by liming and lowered by acidification. Liming is the process
          of adding any material to the acid soil for the purpose of neutralising it in order to
          create a favourable condition for plant growth and microbial activities. Substances
          which are commonly used for liming are calcium and magnesium salts of weak
          acids and basic compounds such as oxides of calcium and magnesium. Oxides and
          carbonates of calcium  and magnesium are called agricultural  limes. When such
          substances are added to the acidic soil, they raise the exchangeable cation level in
          the soil. Acidification is the build-up of hydrogen cations which reduces the soil
          pH. This is done by adding ground sulphur, sulphuric acid, phosphoric acid, ferrous
          sulphate or aluminium sulphate. These materials are, however, always expensive
          and unpleasant to handle.

          Note:  Where it is not possible to correct soil pH at all due to various reasons, for
                 example, economic constraints, crops tolerant to an existing soil reaction
                 may be grown with advantage. To implement this, you should have to seek

                 advice from your local extension worker or other agricultural experts.

          Activity 2.1
          Perform the following tasks.
          1.  Collect soil samples from different areas at your school farm and determine
              their pH using different methods by following procedures you have learnt.

          2.  Outline the lessons you have learnt from this activity.


          Carbon to nitrogen ratio
          Carbon to nitrogen ratio is closely related to breakdown or decomposition of organic
          matters in the soil. It is defined as a ratio of the mass of carbon to the mass of
          nitrogen in organic residues. Carbon to nitrogen ratio is abbreviated as C/N or C:N
          ratio. The C/N ratio of a material is obtained by dividing the mass of carbon by that
          of nitrogen of a particular material. The C/N ratio is generally greater than one,
          that is, organic residues have more carbon than nitrogen. So, it is often written as a

          number; not as a ratio.

          The mass of carbon and nitrogen in a material is determined by using an elemental
          analyser machine. However, the machine method is quite sophisticated and expensive.

                                                                    Student’s Book Form Three
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