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Chapter


                  Two



                             Chemical properties of soil



                    Introduction
          In previous classes, you learnt about physical properties of soil and their importance
          in agricultural production. In this chapter, you will learn about the concept of chemical
          properties of soil, soil colloids, ion exchange, soil pH and carbon to nitrogen ratio
          in relation to soil fertility and productivity. The competencies developed from this
          chapter will enable you to manage soil properly so as to attain maximum returns
          from soil.


          The concept of chemical properties of soil

          Chemical properties of soil can be described as interactions of various chemical
          constituents that take place among soil particles in the soil solution. The levels and
          availability of nutrient elements to plants is an essential component of chemical
          properties of soil. Thirteen (13) out of sixteen (16) nutrient elements are obtained by
          crop plants from soil mineral or organic matter and they can be restored by application
          of manures or fertilisers. All these nutrients are taken up in ionic forms from the

          soil solution as cations or as anions. These include nitrogen (N), phosphorus (P),
          potassium (K), calcium (Ca), magnesium (Mg), sulphur (S), iron (Fe), manganese
          (Mn), zinc (Zn), boron (B), copper (Cu), molybdenum (Mo) and chlorine  (Cl).
          Three (3) out of the sixteen (16) nutrient elements are obtained by crop plants from
          air and water. These nutrients are carbon (C), hydrogen (H) and oxygen (O). Even
          though we don’t apply manure or fertiliser materials to the soil in order to supply
          carbon, hydrogen and oxygen; soil management practices affect their availability.
          The basic factors related to levels and availability of nutrient elements to plants
          include soil colloids, ion exchange, soil pH and Carbon to Nitrogen ratio. These

          factors are discussed in the following sections.

          Soil colloids

          You have learnt in previous classes that soil consists of solid particles of different
          sizes which are generally large, intermediate and very small or mixture. Some of
          those particles are clay and humus. Clay and humus particles are very small in size.


                                                                    Student’s Book Form Three
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