Characterization, classification, and suitability evaluation of soils formed in fluvial deposits within eastern part of Kogi State in Nigeria for rice and maize production

M. Ukabiala, P. Ezeaku, J. Kolo, C. P. Umeugokwe, F. Okenmuo
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Abstract

The impact of rice and maize production on food security in Nigeria cannot be over-emphasized. The aim of this research was to characterize, classify and evaluate the suitability of soils formed in fluvial deposits within eastern part of Kogi State in Nigeria for rice and maize production. This was supported by the fact that the knowledge of the characteristics and soil groups of fluvial deposits in soils is an integral part in soil suitability evaluation as well as management. Four (4) soil profile pits were sunk within the research area. The pedonswere located within the 19a mapping unit of the soil map of Nigeria which has the fluvial deposits. Pedons were adequately described as soil samples were collected from pedogenic horizons, and preserved in well-labelled polyethylene bags, transported to the Laboratory for analyses. The findings revealed that the soils were characterized by dominant gray (10YR4/1) and dark reddish gray (10R4/1) in the surface soils and dominance of various shades of gray in the subsurface soils. Most of the soil structures were single-grained and subangular blocky at the surface and subsurface soils respectively. The soil texture was sandy clay loam and sandy loam in the A horizons. The soil reaction showed mean values of 6.1 and 5.5 at the surface and subsurface horizons with base saturation highest (91%) at C1 horizon of 19a3 pedon. The pedons were classified as inceptisols, and were currently not suitable (N1) for rice cultivation but marginally suitable (S3) for maize cultivation.
尼日利亚科吉州东部河流沉积物中形成的适于水稻和玉米生产的土壤的特征、分类和适宜性评价
水稻和玉米生产对尼日利亚粮食安全的影响怎么强调都不为过。这项研究的目的是表征、分类和评价尼日利亚科吉州东部河流沉积物中形成的土壤是否适合种植水稻和玉米。对土壤中河流沉积物的特征和土壤群的了解是土壤适宜性评价和管理的一个组成部分,这一事实支持了这一点。在研究区内共挖了4个土剖面坑。这些土堆位于尼日利亚土壤地图的19a绘图单元内,该单元有河流沉积物。土样被充分地描述为土壤样本是从成土层收集的,并保存在标记良好的聚乙烯袋中,运送到实验室进行分析。结果表明,该地区表层土壤以灰色(10R4/1)和深红灰色(10R4/1)为主,地下土壤以各种深浅灰色为主。土壤结构在表层和地下分别以单粒和亚角块状为主。A层土壤质地为砂质粘壤土和砂质壤土。土壤反应在地表和地下的平均值分别为6.1和5.5,其中在19a3土层C1层的碱性饱和度最高(91%)。分类为初殖螟,目前不适合水稻种植(N1),但略微适合玉米种植(S3)。
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