Browsing by Author "Kebeney, S. J."

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Effects of nitrogen fertilizer rates and soybean residue management on nitrate nitrogen in sorghum-soybean intercropping system
(SCIENCEDOMAIN international) Kebeney, S. J.; Semoka, J. M. R.; Msanya, B. M.; Ng’etich, W. K.; Chemei, D. K.
Effects of nitrogen fertilizer rates and soybean residue management on nitrate nitrogen in sorghum-soybean intercropping system
(SCIENCEDOMAIN international, 2014-10-11) Kebeney, S. J.; Semoka, J. M. R.; Msanya, B. M.; Ng’etich, W. K.; Chemei, D. K.
An experiment was carried out in Busia County, Kenya at Emalomba (N 00°25′28.8″ E 034°15′ 51.9″), Nambale District to assess the effects of nitrogen fertilizer rates and legume management options on nitrate nitrogen (NO3-N) under intercropping system. Six soybean residue management options were considered: Sole sorghum, sorghum + soybean left to maturity, sorghum + soybean mulched, sorghum + soybean incorporated, sorghum + soybean exsitu and sorghum + soybean exsitu and plot tilled. Three levels of nitrogen (0kg N ha-1, 40kg N ha-1, and 80kg N ha-1 as urea were applied as top-dress and treatments arranged in randomized complete block design. Soil NO3-N was significantly high (P<0.0010) in topsoil with a notable leaching to subsoil due to precipitation. Control treatments had low soil NO3-N in comparison to other treatments implying that, use of inorganic fertilizers to supplement soil N is important. Fertilizer application at 40kg N ha- 1 with respect to on-farm soybean residue management was in relation to NO3-N supply was in the order: sorghum + soybean left to maturity > sorghum + soybean mulched = sorghum + soybean incorporated. Experimental plots with legume residues removed had significantly (P<0.001) low NO3-N. High leaf NO3-N observed points to transfer of N to sorghum by nitrogen fixation signifying importance of intercropping. There was no significant difference between nitrogen fertilizers applied at 40kg N ha-1 and 80kg N ha-1 irrespective of field managed legume residues. Sorghum intercropped with soybean left to maturity with nitrogen fertilizer applied at 40 kg N ha-1 reflected high (P< 0.001) soil NO3-N in comparison to the other management options. It is therefore recommended as a possible optimum rate and legume residue management option to improve soil NO3-N among small scale households with stretched socio-economic ability in Busia County.
Influence of soybean residue management on nitrate nitrogen accumulation and subsequent sorghum yield in Kanhaplic Haplustults of Western Kenya
(Journal of Agriculture and Ecology Research International) Kebeney, S. J.; Semoka, J. M. R.; Msanya, B. M.; Ng’etich, W. K.
Influence of soybean residue management on nitrate nitrogen accumulation and subsequent sorghum yield in Kanhaplic Haplustults of Western Kenya
(Journal of Agriculture and Ecology Research International, 2017) Kebeney, S. J.; Semoka, J. M. R.; Msanya, B. M.; Ng’etich, W. K.
Crop residues are overlooked when making fertilizer recommendations, yet have potential to contribute to soil nitrogen in addition to mineral fertilizer use. A study was carried out in western Kenya to establish the contribution of soybean residues under varied management options and nitrogen fertilizer rates on nitrogen supply to subsequent sorghum crop. Six soybean residue management options were evaluated; sole sorghum, sorghum + soybean left to maturity, sorghum + soybean mulched, sorghum + soybean incorporated, sorghum + soybean exsitu and sorghum + soybean exsitu and plot tilled. Three levels of nitrogen (0 kg N ha -1 , 40 kg N ha -1 , and 80 kg N ha -1 ) as urea were applied as top-dress and treatments arranged in randomized complete block design. -1 Soybean left to maturity at 40 kg N ha indicated significant (P < 0.001) increase (56%) in soil NO 3 -N. Removal of soybean residues resulted in significantly (P < 0.001) lower soil NO 3 -N increase while control treatment and sole sorghum indicated the lowest soil NO 3 -N accumulation irrespective of nitrogen fertilizer rates. Soybean left to maturity indicated significant (P < 0.001) increase (43%) -1 in leaf NO 3 -N accumulation at 40 kg N ha while treatments with soybean residues mulched showed 39% increase and those with residues incorporated, 25% increase. Soybean residues ex- situ and ex-situ and till indicated a decrease (-6% and -7%) in leaf NO 3 -N accumulation, respectively. Sole sorghum had a uniform NO 3 -N increase of 4% irrespective of nitrogen fertilizer rates. It was observed that insitu soybean residues and nitrogen fertilizer application had no significant (P < 0.05) influence on sorghum yield. In conclusion, soil and leaf NO 3 -N accumulation by soybean residues in addition to nitrogen fertilizer does not translate to optimum nor potential research sorghum yields. There is need to research on sulphur and nitrogen to establish their interactive effects on sorghum yields.
Pedological characterization of some typical soils of Busia county, Western Kenya: soil morphology, physico-chemical properties, classification and fertility trends
(International Journal of Plant & Soil Science) Kebeney, S. J.; Msanya, B. M.; Ng’etich, W. K.; Semoka, J. M. R.; Serrem, C. K.
Pedological characterization of some typical soils of Busia county, Western Kenya: soil morphology, physico-chemical properties, classification and fertility trends
(International Journal of Plant & Soil Science, 2014-09-06) Kebeney, S. J.; Msanya, B. M.; Ng’etich, W. K.; Semoka, J. M. R.; Serrem, C. K.
Standard soil survey was carried out in Western Kenya to establish representative research sites on the basis of landforms and other physiographic attributes. Soil profiles were characterized at Emalomba (Nambale District) designated (EMA-P1) and at Bukhalalire (Butula District) named BUMA-P1. Both pedons formed from in-situ weathering of granitic rocks under ustic moisture and iso-hyperthermic temperature regimes. Fourteen soil samples from genetic horizons were analyzed for physico-chemical properties. Both pedons had dark brown sandy clay and sandy clay loam topsoils overlying dominantly clayey subsoils. Both pedons indicate clay eluviation-illuviation as a dominant pedogenic process with strong acidic soil conditions and available phosphorus of < 7 mg/kg soil. Organic carbon (OC) is high in EMA-P1 and medium to very low in BUMA-P1 while total nitrogen is medium and low to very low. EMA-P1 and BUMA-P1 have C/N ratios of 8.6 - 9.6 and 12.9 - 24.8 respectively. Both pedons have low to very low exchangeable bases with cation exchange capacity (CEC) < 16 cmol(+)/kg soil. CEC clay values in both pedons are < 24 cmol(+)/kg with BUMA-P1 having < 10 cmol(+)/kg. Both soils are highly weathered with BUMA-P1 depicting more advanced stage of weathering. In the USDA Soil Taxonomy, EMA-P1 was classified as Kanhaplic Haplustults and BUMA-P1 as Typic Kandiustults, both corresponding to Haplic Cutanic Acrisols in WRB. As regards soil fertility trends, OC showed positive correlation with calcium and magnesium indicating organic matter as the main source of plant nutrients. The two pedons differed noticeably in terms of physico-chemical characteristics emphasizing the need to characterize soils before fertilizer recommendations are made. Organic fertilizers are recommended to increase organic matter content and intercropping of cereals with nitrogen fixing legumes to enhance nitrogen in the soils. Use of non-acidifying inorganic fertilizers and lime as soil amendments should also be considered to correct acidity.
Socioeconomic factors and soil fertility management practices affecting sorghum production in Western Kenya: a case study of Busia county
(American Journal of Experimental Agriculture) Kebeney, S. J.; Msanya, B. M.; Semoka, J. M. R.; Ng’etich, W. K.; Kipkoech, A. K.