Introduction to soil fertility
Soil fertility is a concept based on the amounts of essential
nutrients available to the plants. The plant nutrients involved are classified
as macronutrients such as nitrogen (N.), phosphorous (P), potassium (K), calcium
(Ca), magnesium (Mg), and sulfur (S); or as micronutrients such as i iron (Fe),
manganese (Mn), copper (Cu), zinc (Zn), boron (B), and molybdenum (Mb). The
amount of each of these nutrients is not the only factor in determining whether
there are nutrient shortages. Soil pH (acidity) is also important because under
certain pH conditions, nutrients form insoluble compounds which are unavailable
to be taken up by plant roots. A shortage of any of these elements in the soil
can slow crop development and reduce yields, something which extentionists
should consider when working with farmers to improve crop production.
In practice, soil fertility is determined by collecting a soil
sample and submitting it for chemical analysis. Since a small sample will be
used to infer the characteristics of an entire field, care should be taken to
ensure that the sample represents as accurately as possible the conditions
present in the plot.
Sampling may be done with a soil probe or a shovel, being
careful to exclude the surface litter layer and sampling at a depth of
approximately 1"-8" below the surface. Subsamples should be taken from random
positions throughout the entire field (10-20 per hectare) and mixed thoroughly
in a bucket or bag. From this mix, a 1-2 lb. sample is air dried, labelled, and
submitted to a laboratory for analysis. A highly variable field should be
subdivided into fairly uniform sections which should each be treated separately,
as they may have very different soil characteristics. Samples may be analyzed
with portable field test kits, if available, but it is also advisable to
familiarize farmers with the laboratory facilities available to them. In
Honduras, for example, soil analyses are performed at the laboratories of
Recursos Naturales in Tegucigalpa, Standard Fruit Company in La Ceiba, the
Escuela de Agricultura Panamericana in El Zamorano Valley and FHIA in La Lima,
Cortes. The most common soil analyses performed are those for nitrogen,
phosphorous, potassium and pH, which generally are most important in limiting
crop yields. If crops do not appear to respond to changes in these factors then
perhaps a deficiency of another nutrient is involved and a mere detailed
analysis can be carried
out.