Abstract:
.
Iodine is beneficial in human nutrition and to a lesser extent in plant nutrition. Availability of this element in the soil is thought to be via ocean-atmosphere precipitation, iodine minerals and redistribution by vegetation, but very little is known about levels of iodine in Ghanaian soils. We analyzed for the content of total iodine alongside pH, organic carbon, total nitrogen, cation exchange capacity, sand, silt and clay in top soils of selected agro-ecological zones. These soils occur at various locations spanning from the coastline to the far interior. Variations in nutrient elements were attributed to diverse parent materials from which these soils originated and the complex interactions of organic matter, type of clay, acidity-alkalinity and leaching processes. The soils recorded low total iodine content of 0.08 – 3.92 µg g-1. There was a decreasing trend of iodine from the coastal zone inwards in the order of 1.85, 0.84 and 0.66 µg g-1 for the coastal savanna, semi-deciduous rainforest and Guinea savanna agro-ecological zones respectively. Iodine very weakly negatively correlated with C and N and showed a moderate positive correlation with clay content and moderate negative correlations with pH and sand content
