Research was carried out at University Commercial Crop Farm, Federal University of Agriculture Makurdi, to evaluate the effects of different soil nutrient sources on the growth and yield of sorghum in the 2016 and 2017 cropping season under rain-fed condition. The experiment consisted of fourteen treatments; (I) Control, (II) Soybean intercrop, (III) 2.0 t/ha-1 of PM, (IV) 2.0 t/ha-1 of PM + Soybean, (V) 3.5 t/ha-1 of PM, (VI) 3.5 t/ha-1 of PM + Soybean, (VII) 0.2 t/ha-1 of CP, (VIII) 0.2 t/ha-1 of CP + Soybean, (IX) 0.4 t/ha-1 of CP, (X) 0.4 t/ha-1 of CP + Soybean, (XI) 30 kg N/ha-1, (XII) 30 kg N/ha-1 + Soybean, (XIII) 60 kg N/ha-1, and (XIV) 60 kg N/ha-1 + Soybean. The experiment was laid in Randomised Complete Block Design in three (3) replications. Sole applications of compost manure at 0.4 t/ha-1 had significant difference on leaf area. Soybean as nutrient source did not have significant difference on crop parameters. Poultry manure, NPK fertilizer and compost manure significantly affected growth and yield parameters in the two cropping seasons. The highest yield were obtained from application of NPK fertilizer at 60 kg N/ha-1 in plots where sorghum was intercropped with soybeans, this was not however significant when compared with plots where NPK fertilizer was applied without soybean mixture.
Ultisols in Benue state were studied to determine the solution phosphate concentration (SPC) required to obtain optimum yield of soybean for estimating the P fertilizer requirement of soybean. Soil inorganic P was fractionated using standard procedures. Sorption characteristics were determined in 0.01 M CaCl 2 solutions of various P concentrations. Amounts of P that gave 0. 025, 0.05, 0.075, 0.100, 0.125, 0.150, 0.175, 0.200, 0.225, 0.250
Phosphorus (P) sorption influences P requirement of Nigerian soils. Four Inceptisols in Benue state were therefore used to examine the influence of soil properties on sorption indices and yield of soybean. Soil inorganic P was fractionated using standard procedures. Sorption characteristics were determined in 0.01 M CaCl 2 solutions of various P concentrations. For each soil, the amounts of P that gave 0
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