Soil is the natural medium in which crops grow. Under the Kenyan Senior School CBC (KICD) Agriculture pathway, you learn how to read soil so that you can choose the right crop and management practice for your farm or school garden.
Soil is made up of:
Soil texture refers to the relative proportions of sand, silt and clay.
Soil structure is how particles clump into crumbs. Good crumb structure allows air and water movement and root growth. Porosity is the amount of pore space, and soil temperature affects germination and microbial activity.
Soil pH measures acidity. pH 7 is neutral, below 7 acidic, above 7 alkaline. Most crops prefer pH 6.0 to 7.0. Tea, however, prefers acidic soils (pH 4.5 to 5.5), which is why it thrives in Kericho and Nandi. Cation exchange capacity is the soil's ability to hold nutrients such as potassium and calcium.
A soil profile is a vertical section showing layers called horizons:
A fertile soil supplies nutrients in adequate amounts and balance. Farmers maintain fertility by:
A soil sample has 40% sand, 40% silt and 20% clay. Which texture is it? Answer: None of the three dominates strongly, so it is a loam, suitable for maize and vegetables.
A farmer in Kiambu finds soil pH 5.0 but wants to grow beans (pH 6.0 to 7.0). What should he do? Answer: Apply agricultural lime (calcium carbonate) to raise the pH, then retest after a season.
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