尼日利亚东科吉河尼日尔河冲积平原部分土壤的特征、分类和适宜性评价,用于水稻、玉米、木薯和油棕的生产

M. Ukabiala
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摘要

本研究对科吉东部尼日尔河沿岸的4种土壤进行了特征、分类和评价,用于水稻、玉米、木薯和油棕的生产。土壤主要由冲积层发育而成。土壤分布在科吉东部尼日尔河漫滩的Ejule-Ojebe、Shintaku、Bagana和Kpata四个社区。采用自由测量法对土壤进行了调查。研究了位于河漫滩不同地点的四种土壤的四个土墩。根据标准的现场程序对环境和土壤剖面进行了描述。然后从遗传层提取土壤样本进行实验室分析。根据《土壤分类》和《世界土壤资源参考基础》(WRB)对土壤进行了分类。由于排水不良,土壤的颜色从深浅不一的棕色到灰色不等。由于剖面发育的不同,土壤的深度和水平也不同。由于土壤含沙量相对较高,特别是在表层和地下层,土壤的质地一般为砂质至粘壤土。土壤pH (H2O)值在4.8 ~ 7.3之间,呈强酸性到微碱性,且随深度增加呈增加趋势。表层土壤有机碳含量适中,下层土壤有机碳含量较低。根据土壤的性质,将土壤分类为Alfisols (Ejule-Ojebe)、Entisols (Shintaku)、Inceptisols (Bagana)和Alfisols (Kpata);根据WRB将土壤分类为Planosols、Arenosols、Gleysols和Planosols。土壤非常适合种植水稻,但中等适合种植玉米、木薯和油棕。除水稻种植外,土壤湿度是玉米、木薯和油棕最佳旱作栽培的主要限制因素。
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Characterization, classification, and suitability evaluation of some soils in the floodplains of River Niger, Kogi East, Nigeria for rice, maize, cassava, and oil palm production
This study was conducted to characterize, classify and evaluate four soils along River Niger in Kogi East for rice, maize, cassava and oil palm production. The soils developed predominantly from alluvium. The soils were located in four communities namely Ejule-Ojebe, Shintaku, Bagana and Kpata all in the floodplains of River Niger in Kogi East. The soils were investigated using a free survey technique. Four pedons representing four soils located at different sites in the floodplain were studied. The environs and the profiles of the soils were described according to standard field procedures. Soil samples were then taken from genetic horizons for laboratory analysis. The soils were also characterized and classified according to Soil Taxonomy and the World Reference Base for Soil Resources (WRB). The colour of the soils ranged from shades of brown to grey generally due to poor drainage. The soils also varied in depth and horizonation due to differences in profile development. Due to the relatively higher sand content of the soils, especially in the surface and subsurface horizons, the texture of the soils generally ranged from sand to clay loam. The pH (H2O) of the soils ranged from 4.8 to 7.3, strongly acidic to slightly alkaline, and tended to increase with depth. The soils containedmoderate amounts of organic carbon in the surface soils but lower levels in the lower horizons. Based on their properties, the soils were classified according to Soil Taxonomy as Alfisols (Ejule-Ojebe), Entisols (Shintaku), Inceptisols (Bagana) and Alfisols (Kpata) and according to WRB as Planosols, Arenosols, Gleysols and Planosols, respectively. The soils were found to be highly suitable for rice production but moderately suitable for maize, cassava and oil palm. Apart from rice cultivation, wetness of soil was found to be the major limiting factor for optimum rainfed cultivation of maize, cassava and oil palm.
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