Calcaric Cambisol (WRB 1998)
Soil is developed from colluvial deposits derived from basic gneiss. Few to common calcium carbonate nodules present at about 50cm from surface.
Chromic Luvisol (WRB 1998)
Soil is a sedentary soil developed over quartz sericite schist. It contains a few gravel in the upper 20 cm or so, but dominantly Gravel and stony in the sub-soil.
Stagnic Luvisol (WRB 1998)
Soil is developed on colluvial materials derived from acidic gneiss. Effective soil depth to perched water table is at 80 cm.
Thaptoplintic-Eutric Cambisol (WRB 1998)
The soil is developed in colluvial material derived from acidic gneiss. Materials suspected to be plinthite occur between 124 and 150 cm. Evidence of lithological discontinuity was observed below 56 cm from soil surface.
Demonstration of conservation agriculture tools utilization in Kenya (FAO, project) during the 3rd World Congress on conservation agriculture - LT, 2005).
Soil erosion impact on water quality in Burkina Faso -LT July 2005
Soil pollution by plastics along the Volta river in the transboundary area Ghana/Burkina Faso - LT July 2005
