HomeAnnals of Tropical Researchvol. 44 no. 1 (2022)

Assessment of sesquioxides status of some uplands soils in humid southwest Nigeria

Julius Olayinka Ojetade | Emmanuel Adeboye Adesemuyi | Alani Adeagbo Amusan | Ruth Oluwakemi Adegbenro | Sikiru Adekoya Muda

 

Abstract:

Assessment of some sesquioxides in the upland soils in southwestern Nigeria was undertaken to evaluate their degree of weathering under humid tropical conditions. Samples were taken from genetic horizons of eight soil profile pits sited at different physiographic positions along two toposequences in southwestern Nigeria. The samples were analyzed for gravel content, particle size distribution, bulk density, pH, organic carbon, total nitrogen, available P, exchangeable bases, crystalline and amorphous forms of Fe and Al, using standard procedures. Sand fraction ranged from 31–76% (54.49±11.34), silt from 3–19% (10.21±3.61) and clay from 10–55% (35.3±9.7). Bulk density increased with profile depth, ranging between 1.12 and 1.64g cm (1.39 0.13). pH was low (4.2–6.1; 5.0 0.55), organic -3 ± The ± carbon content ranged from 0.75–15.99g kg (5.79 3.49) with higher values in the -1 ± surface horizons. Total nitrogen content ranged from low to medium (0.13–2.75g kg ; 1.16 while available phosphorus ranged from 0.49–11.63mg kg -1 -1 ±0.49) (4.30±3.57) across the horizons. Crystalline forms of Fe (Fe ) and Al (Al ) ranged d d from 10.26 39.82 and 0.41 1.80 , respectively while the amorphous -1 -1 – g kg – g kg forms (Fe an Al ) ranged from 0.41 2.60 and 0.83 1.64 respectively. o o d -1 -1 – g kg – g kg , The crystalline forms of Fe and Al were more dominant over the amorphous forms d d of Fe and Al . The a s d o o rgillic (Bt) horizon of pedons ha significant accumulation of clay particles and free iron. The weathering indices of clay and free iron accumulation in argillic (Bt) horizons of the pedons indicated that the soils of the study area were well-drained, deeply weathered and intensely leached with few weatherable minerals available for plant uptake.



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